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Shirley Peruniak: Quetico Park Naturalist

Originally published June 10th 2004, revised January 25, 2010

Shirley Peruniak: Quetico Park Naturalist

Shirley Peruniak: Quetico Park Naturalist

With the opening of Highway 11 from Thunder Bay to Atikokan in 1956, there was, for the first time, road access to the northern part of Quetico Park. One of the people who drove that road and started a canoe trip at French Lake that summer was a young woman named Shirley Peruniak. That canoe trip was the beginning of a love affair with Quetico that is still going strong today.

Shirley officially retired sixteen years ago after nineteen years as a Quetico Park naturalist. Fortunately for the park, even though she has retired, her ongoing quest to explore and gather information about Quetico continues. Her research into Quetico’s past culminated in the publication of Quetico Provincial Park: An Illustrated History in 2000.

Dave Elder, a former Quetico Park superintendent, calls Shirley the “heart and soul of Quetico”. Everybody who knows Shirley would agree with this assessment of her. She has definitely poured her heart and soul into her work in Quetico and her impact on co-workers in the park and park visitors has been profound.
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Quetico Park: Twelve Thousand Years in the Making – A Century of Protection

Quetico is celebrating its 100th Anniversary. Quetico was originally set aside in 1909 as the Quetico Forest Reserve, became a Provincial Park in 1913, logging was banned in 1972 and it was declared a wilderness park in 1978. Quetico is characterized by towering cliffs, rocky islands and sandy beaches in a watery landscape of clear water lakes, rivers, creeks and bogs. These compelling attributes that attract canoeists to Quetico are primarily the results of the actions of glacial ice and glacial meltwater at the end of the last Ice Age.

Silver Falls at dusk the day after ice-out in 2008.

Continue reading ‘Quetico Park: Twelve Thousand Years in the Making – A Century of Protection’

Excerpts from chapters in Quetico: Near to Natures Heart.

Prelude (excerpt)

QUETICO — ONE HUNDRETH ANNIVERSARY
OF A “MAGIC LAND”

In 1909, Ernest Oberholtzer, a pioneer in preserving the Quetico-Superior region, made a canoe trip in Quetico with his Ojibwa friend Billy Magee. They saw moose almost every day; they were intrigued by the pictographs they encountered; they marvelled at the beauty of Rebecca Falls and Sue Falls; and they saw large stands of old pine, including a white pine on Jean Lake that they estimated to be one and one-half metres (five feet) in diameter. This was Oberholtzer’s first extensive trip into the Quetico-Superior region and the experience inspired him to dedicate his life to preserving its wilderness character.

As Oberholtzer and Magee zigzagged across Quetico, in addition to the wondrous scenery and wildlife, they found many examples of human impact on the landscape. They saw foundations for the Hudson Bay Company post on the Pickerel Lake to Dore Lake portage, dams on the Maligne and Knife rivers, a logging camp on the Knife River, and a trading post on Basswood Lake. They also talked to rangers patrolling for poachers and putting out fires. And on numerous occasions they encountered Ojibwa people. During their journey they noticed pole structures for spearing sturgeon on the Namakan River; saw cedar strips drying for baskets and bear pelts hanging on racks at Lac La Croix; stayed on a site where birchbark canoes were made on Poohbah Lake; and came upon an Ojibwa couple in a birchbark canoe using a blanket for a sail on Kawnipi Lake.

Recalling his trip years later, Oberholtzer recalled that Quetico in 1909 was such a special place that the Indians felt “that there is a spiritual power back of it all.” He noted that “it was no wonder that they had traditions and felt spirits in there, it had a spirituality about its appearance, you felt you were in kind of a magic land.”

Native peoples have a long history in Quetico. Over twelve thousand years ago, near the end of the last ice age, Palaeo-Indians moved into the area. They were followed by a series of Native cultures culminating with the Sioux, Cree, and, finally, the Ojibwa, who inhabited the area when the first white settlers arrived. Those settlers, some of whom remained in the Quetico-Superior, were part of a diverse group of people that began traversing this terrain in the 1600s: European explorers searching for the Pacific Ocean, voyageurs transporting trade goods and furs, and surveyors and geologists paving the way for settling the area west of Lake Superior. As well, Grey Nuns travelling to Winnipeg in 1844 to set up a school; the 1870 Wolseley expedition to quell the Riel Rebellion in Manitoba; settlers heading west along the Dawson Route; and trappers, park rangers, poachers, timber cruisers, loggers, and miners all comprise just a small sample of those who have moved along Quetico’s waterways after the arrival of the Europeans.

One hundred years after Quetico was first set aside, we walk many of these same portages and pitch our tents on the same campsites where everyone from Paleo-Indians to Oberholtzer and Magee spent the night. We are fortunate that Quetico was protected early enough that its combination of a glorious, mainly undisturbed, landscape and its long and varied human history still retains the magic that Oberholtzer found in 1909.

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Chapter Two (excerpt)

PALAEO-INDIANS:
FIRST EXPLORERS OF THE QUETCIO-SUPERIOR

The first people to enter the Quetico-Superior area encountered a landscape rubbed raw by glacial ice, witnessed glaciers calving into an inland sea, and crossed a landscape devoid of trees.1 The earth was recovering from an ice age and a massive continental glacier was melting and receding northward. These first explorers, known as Palaeo-Indians, entered a landscape that had recently been populated by vigorous, cold-adapted plants and animals. They were following herds of barren-ground caribou that grazed on succulent tundra plants. In the southern part of the Quetico-Superior area, woolly mammoths and mastodons may also have been prey for these highly mobile big-game hunters who had the technology and skills to thrive in a changing and often hostile, environment.

Since the continental glacier was receding, much of the area was flooded by glacial meltwater that formed glacial Lake Agassiz. The first people to enter the Quetico-Superior region probably came into the higher elevation areas in the eastern part of the BWCAW and moved north into the eastern part of Quetico Park. As the glacier continued to recede and the water level of Lake Agassiz dropped, they then moved into the rest of the area.

The Palaeo-Indians entered this new land as members of small groups that were essentially extended families. Because their prey was mobile, they had to move quickly and often. They also had to find plants for food and medicine, build shelters, make and repair clothing, find stone for tools, and care for the young, the sick, and the elderly as they travelled. Since they were the first explorers of this region, there were no maps, no guides, and no one to ask for advice as to what lay ahead. They experienced the joys and terrors of entering a fresh, new, unexplored land. The information they needed was carried in their heads and they relied on their companions and their collective know-how for survival. They were intrepid explorers of the first magnitude, but neither their names nor the time of their arrival is known.

Exploration and Imagination

Douglas Preston, an American author who has written extensively about North America’s past,
has noted: Sometime during the last Ice Age, a seemingly trivial event took place, one that would change human history forever: a human being first set foot in the new world. We do not know where this person came from, or why, or where the first footfall landed on the New World. Unlike the first man to walk on the moon, the unknown pioneer who made this giant step for mankind was probably not aware of doing anything significant at all, perhaps just taking one more weary stride on a long tramp across the frozen tundra, searching for game. But in that moment, a Garden of Eden of vastness and splendor fell to our species. It would be the last inhabitable area of earth to be occupied by human beings. Not until we colonize the stars will an event of comparable significance take place.

The first people to enter the Quetico-Superior area were a continuation of the exploration of a part of North America just released from the glacier. Since we don’t know the time, the location, or the names of the first explorers of this magnificent part of North America, there is a tendency to minimize the significance of what they did or even ignore them completely. While we rightly celebrate the accomplishments of Pierre Radisson, Jacques de Noyen, Sieur de la Vérendrye, Alexander Mackenzie, Simon Fraser, David Thompson, and other Europeans who explored a land new to them, but one that had been inhabited for thousands of years, we overlook those who came first. I find it exhilarating to be able to travel over portages and sleep on campsites that were used by the first people to enter this area. When paddling on Pickerel Lake, imagine what it would have been like when Lake Agassiz stretched all the way to the prairies and tundra grasses grew in abundance along the shore. Curlews were flying overhead and barrenground caribou travelled along a moraine where red pine and Jack pine now flourish. Palaeo-Indians gathered around a small campfire eating arctic hare and cattail stew seasoned with wild ginger while retelling their grandfathers’ stories of woolly mammoths and huge wolves.

For thousands of years, the descendents of these Palaeo-Indians called the Quetico-Superior region home and sought plants for their medicinal value; caribou, berries, whitefish, moose, and wild rice for food; stone outcrops for tools; wood for dwellings, atlatls, and arrow shafts; and birchbark for containers and canoes. Although twelve thousand years of Native people living off the land ensures that there aren’t many places where no one has been, Quetico is still a land that invites exploration. The joy is in having such a magnificent place to explore. It is always exciting to see a moose feeding in the shallows, discover an osprey nest on a seldom-visited lake, find a calypso orchid, or gaze in wonder at pictographs that hint of an earlier and strikingly different time. Every portage leads to new possibilities. For over forty years I have marvelled at discovering places and objects in Quetico that have been seen by many others — but are new to me.

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Chapter Eleven (excerpt)

THE ORCHID AND THE FUNGUS:
SYMBIOTIC PARTNERS

While portaging my canoe across a flat, rocky portion of the Silver Falls portage between Cache Bay and Saganagons Lake, I looked down and noticed an unusual, multicoloured flower growing just inches from the edge of the trail. Although not far from the descent to Saganagons Lake, I welcomed an excuse to put the canoe down, rest for a moment, and examine the flower that had caught my attention. To my amazement it was a Calypso orchid, an elusive plant I had been searching for for many years. Having always looked in swamps and wet areas where I thought orchids should grow, I was astonished to find one growing in a dry, relatively barren area where hundreds of people must have nearly stepped on it. The combination of small size and relative rarity makes the Calypso orchid a difficult plant to find in Quetico. Distinguished by its vivid colouring and intriguing shape, it is also known as the fairy slipper orchid. The plant is only a few inches tall, but the small flower is simply stunning.

My fascination with orchids and symbiotic relationships began when I saw that Calypso orchid unexpectedly growing along the Silver Falls portage. I couldn’t help but wonder why this orchid was growing in such an unlikely place and why there was just one. Since orchids are primarily tropical plants, there had to be something special occurring to allow this plant, and orchids in general, to grow in cold northern forests.

A Bit of the Tropics in the Quetico-Superior

Orchids are not only sexy and beautiful, they are also a clear and dramatic case of plants that are totally dependent on fungi for their very survival. The symbiosis between orchids and soil fungi makes it possible for plants that are more at home in the hot, moist conditions in the tropics to grow in the Quetico-Superior.

Although orchids require fungi for seed germination, the “infection” by the fungi is apparently greater for northern orchids than for tropical ones. These plants with tiny seeds and intricate, showy blooms need all the help they can get to successfully live so far north. It is the symbiotic interaction between a plant and a fungus that makes it possible for canoeists to see the Calypso orchid, a migrant from the tropics, growing in Quetico beneath boreal trees such as black spruce and Jack pine. As the human impact on the landscape continues to increase, plants that require undisturbed habitats and have other specific needs will become more dependent on wilderness areas such as Quetico Park and the BWCAW for their continued existence.

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Chapter Sixteen (excerpt)

TAILS BENEATH THE SNOW:
LIFE IN THE PUKAK

Geothermal Heat and a Blanket of Snow

For large mammals, including humans, deep snow is a hindrance to travel and survival. When the snow is deep, animals deplete valuable energy resources finding food and avoiding predators. Occasionally, extreme winters can have devastating effects on wildlife. During the winter of 1995–96, exceptionally deep snow caused the populations of white-tailed deer to drop dramatically in both northern Minnesota and northwestern Ontario. That winter, even moose, whose long, stilt-like legs make them well adapted to moving through deep drifts, were dragging their bellies in the snow.

In contrast, deep snow is beneficial for most small mammals. For chipmunks, mice, shrews, and voles, a major threat to their surviving the winter is the lack of sufficient snow rather than too much. Snow actually provides a refuge for them. The small size of these mammals makes them very susceptible to the cold. Hypothermia and freezing to death are constant threats and they have to find a way to avoid the cold if they are to survive the long winters in the Quetico-Superior region. Small mammals use leaf mold, pine needles, and other decaying vegetation as insulation when the temperature plummets. They can also utilize rotting stumps and tangles of downed limbs and branches for both insulation and protection and can burrow into the soil. Snow, however, offers the best protection for these small creatures. Living under frozen flakes seems like an unlikely way to avoid the cold, but snow is actually a very good insulator. Acting as a blanket over the earth, the snow keeps the ground level habitat of the pukak at a liveable temperature.

Fluffy, falling snow is comprised of over 90 percent air and even snow on the ground can contain as much as 70 percent air. It is the air trapped between the crystals that make snow a good insulator. The blanket of snow traps the heat radiating up from deep in the earth and also insulates the ground from the cold air above the snow. When there is no snow, or insufficient snow, the ground heat is lost into the atmosphere.

The amount of snow needed to keep the soil surface temperature near freezing even in the coldest weather — called the heimal threshold — depends on the outside temperature and how packed-down the snow has become. Researchers have found that the snow depth required to reach the heimal threshold varies from twenty to thirty centimeters (eight to twelve inches), depending on the amount of compaction. Quetico Park usually has snow of this depth by late November or early December, but in some winters that depth isn’t reached until much later. When the snow reaches this depth, the temperature of the ground layer stabilizes within a few degrees of freezing, regardless of the temperature of the outside air. The warmth that is constantly radiating from deep within the earth slowly decomposes and sublimates the snow crystals at the base of the snow pack. A latticework of ice columns and openings appears and the naturally occurring openings caused by ground vegetation and leaf litter are enlarged.

The network of openings that make up the pukak forms where there are sufficient herbs and other small plants to keep some of the snow from coming in contact with the ground. This causes small openings or cavities that are added to and enlarged by heat coming up from the ground. Pukak layers vary considerably, depending on the habitat and the conditions as the snow accumulates. A mowed lawn will have virtually no pukak, but most areas with undisturbed vegetation will have a pukak layer as long as there is at least twenty centimetres of snow. Where there is little or no vegetation, and there are many such places in Quetico, no pukak layer forms regardless of the depth of snow. Areas with bedrock at the surface, boulder-strewn shorelines, and the ice surface of ponds and lakes are examples of such places in Quetico where the pukak doesn’t form, regardless of snow depth.

The Mouse and the Moose

Large, bulky creatures, such as humans, are oblivious to the vibrant, thriving communities that live under the snow. An intact web of life — where animals are killed and new life is created — occurs in the vibrant micro-environment under a mantle of snow. In a chapter entitled “Coming of the Snow,” Sigurd Olson lyrically described the pukak world beneath his snowshoes as a “jungle of grassy roots and stems, tiny mountains of sphagnum, forests of heather, the whole interwoven with thousands of twisting burrows of meadow mice.… Theirs was a world removed, an intricate winter community, self-sufficient and well organized.”

The small mammals in the Quetico-Superior area are able to survive, and even thrive, during our long harsh winters by using snow to their advantage. They evade the extreme mid-winter cold by using snow as a blanket, and the earth as a constant source of low heat. They live in an unexpected, surreal environment and have replaced the bitter wind and extreme cold with confined spaces, dim light and constant coolness. When the snow is deep, the moose and the mouse live in the same woods but in very different worlds.


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Quetico: Near to Natures Heart (cover)The book is available at many local bookstores in Ontario and Minnesota. The book is available in Canada from Chapters.Indigo online store or Amazon.ca.

In the United States, the book can be ordered from a variety of sources including Piragis Boundary Waters Catalog, Amazon.com and Barnes and Noble.

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Bob & Leone Hayes: A Quetico Romance

In the spring of 1942, sixteen-year-old Bob Hayes landed at the Bayley Bay Ranger station on Basswood Lake. Years later, he remembers thinking that “I thought I was descending into the ultimate paradise.” Since he was coming from Beaverhouse Lake, where he had worked on a walleye spawning crew, he already knew that working and living in Quetico Park was a perfect fit for a young man interested in the outdoors. He had become quickly infatuated with Quetico, and he soon found out that across the lake was an attraction that proved to be even stronger than Quetico.

Oscar-and-Marie-Johnson

Oscar and Marie Johnson

Leone Johnson, who was also sixteen in 1942, spent her summers working at Johnson Brother’s Fishing Camp, which was owned and built by her father Oscar Johnson and his brother Bill. It was located west of Rice Bay on the American side of the lake almost directly south of the Bayley Bay Ranger Station. Leone’s family has a long history on Basswood Lake. Her father, Oscar Johnson, fished commercially on Pipestone Bay in the 1920’s and he started Johnson Brother’s Fishing Camp with his brother Bill in 1925. The camp, the second one on Basswood Lake, was composed of a main lodge and five cabins. It appealed to serious fishermen and its reputation spread quickly by word of mouth and they never had to advertise. The fishing camp was a family business and Leone worked long hours and had a variety of jobs. Oscar and Bill ran the resort until they sold to the government in 1953 when Basswood resorts were being bought out to create the Boundary Waters Canoe Area Wilderness.

Although Bob’s days were busy with his duties as a Park Ranger, he commonly had time in the evenings to pursue his own interests. Bob was fortunate that both the supervisors he had at Bayley Bay, George Armstrong and Oscar Frederickson, took a liking to him and were willing to assist him in any way they could. For example, on Bob’s first evening on Basswood Lake, George Armstrong took him across Bayley Bay to meet the young women who worked at Johnson Brothers Fishing Camp.

He quickly became smitten with the sparkly-eyed brunette who worked behind the counter. Bob recalls that they were soon “exchanging our life stories, which doesn’t take long when you are sixteen”. Both Bob and Leone recall an “instant chemistry” and they exchanged rings during that summer that “passed all too quickly.”

Bob went back to work on the spawning crew at Beaverhouse Lake in the spring of 1943, but this time he was in charge of the operation. He was just seventeen years old and to make his job more challenging, his twenty-one year old brother was a member of the crew. He went to Pickerel Lake for the first part of the summer where he patrolled for poachers with George Armstrong. Bob had corresponded with Leone over the winter and he was extremely happy to end up back on Basswood Lake for the remainder of the summer. There were many twenty-minute paddles or five-minute boat rides across Bayley Bay during the summers of 1942 and 1943. Bob spent the fall at Cabin 16 on Basswood Lake where he shared the Park Ranger duties with Jess Valley, an experienced Park Ranger. He was able to visit Leone on weekends, traveling by canoe in the fall and by snowshoe in the winter.

In the fall of 1943, World War II was becoming very intense and Bob felt a strong obligation to do his part. Since he was not yet eighteen, he had to get written permission from his parents to join the military. He enlisted in the Royal Canadian Air Force in January of 1944 and quickly came to the realization that he might not survive the war. Since he was unsure of his fate and didn’t want Leone to wait, possibly in vain, for his return, he reluctantly wrote her a ‘Dear Jane’ letter. After his military training, he was sent to England where he served as a flight engineer on a Lancaster Bomber on bombing missions over Germany. He was discharged in the spring of 1946 and quickly discovered that Leone had taken his letter seriously and had married and had a baby.

Bob was anxious about returning to Quetico Park but, for obvious reasons, he had no desire to go back to Basswood Lake. He spent the summer working at Lac La Croix but was assigned to work with Jess Valley again at Cabin 16 on Basswood Lake in the fall. He agreed to go since he knew Jess and enjoyed working with him. When the plane landed on Basswood Lake, Bob learned that Leone’s husband, who was only 26 years old, had just died from congestive heart failure. Bob went to see Leone that fall and they both looked forward to seeing more of each other the next summer on Basswood Lake.

In the spring of 1947, Leone was back working at her parents’ resort near Rice Bay on Basswood Lake and Bob was glad to be back on Bayley Bay working for Oscar Frederickson. Bob describes Oscar as one of the most unforgettable people that he has ever met. He was a man with “a gruff exterior, but a heart of gold.” During the summer, park authorities decided to transfer Bob to Lac La Croix. Oscar Frederickson, however, had other ideas. Bob recalls that Oscar radioed park headquarters, although the plane was already in the air, and growled, “I want Hayes to stay here and here he’s going to stay.” Oscar was highly respected by park officials and his opinion carried a lot of weight. The plane landed, but flew back without Bob.

Bob and Leone saw a lot of each other during the rest of the summer and, to no one’s surprise, decided to get married. Bob quit the Ontario Department of Lands and Forests (the precursor of the Ontario Ministry of Natural Resources) in January of 1948 and married Leone in May of 1948. They moved to Emo, Ontario where Bob worked as a heavy equipment operator for the Department of Highways. They had a daughter, Suzie, two years later. They were content living in Emo, but they both missed northern Minnesota with its proximity to Basswood Lake and felt they would be happier in Winton. Bob contacted the U. S. Consulate in Winnipeg and had his visa in just six weeks. They moved to Winton and Bob was quickly hired to work at the Winton Hydro Electric dam on Fall Lake. He worked there for 31 years and retired in 1985 at the age of 59.

Bob’s Early History

Manitou Rapids Reserve in 1932

Manitou Rapids Reserve in 1932

Bob was born in 1926 and grew up on the Manitou Rapids Reserve, which is located on the north shore of the Rainy River west of Fort Francis, Ontario. His father was the agricultural agent of the Reserve and he was the first white baby born on the Reserve which is now part of the Rainy River First Nation. The Manitou Mounds, situated along the shore of the Rainy River, are the largest group of burial mounds in Canada. This site, known in Ojibwa as Kay-Nah-Chi-Wah-Nung, or “place of the long rapids”, was declared a site of national historic significance in 1970. It is now the home of a terrific Interpretive Centre that presents local history from a First Nations point of view.

Bob and his two brothers had an idyllic childhood growing up along the Rainy River. It must have been similar to my childhood in southern Minnesota except he was fishing for walleyes instead of bullheads and playing “cowboys and Indians” with real Indians.

Leone’s Early History

Leone Johnson on Basswood Lake summer 1942

Leone Johnson on Basswood Lake summer 1942

Leone was born in Ely, Minnesota and lived in Winton until her family moved back to Ely when she was in the sixth grade. She had a typical northern Minnesota childhood except she spent her summers working at her parents resort on Basswood Lake. She started when she was very young and her responsibilities increased as she got older. She cleaned cabins, worked in the kitchen, cut firewood with a cross cut saw, cleaned outhouses, put up ice, and pumped water up to the tank. A small generator powered the resort and it was turned off, and the lights went out, at 10 p.m.

She also had opportunities to get out onto the lake. The resort had launches and, on occasion, she was able to ride on trips to pick up or drop off guests at Four Mile Portage or even take excursions into the Canadian side of the lake to drop canoeists off at the beginning of their trips. Each morning, Leone used to take a boat to Leo Chosa’s store at Prairie Portage to get minnows. Her friends from Ely and Winton also came up to visit. Of course, she also got time off to take part in those pleasant activities, such as fishing and swimming, that go with living on the lake.

Basswood Lake in the 1940’s

The Basswood Lake that Bob landed on in 1942 was a very different place from what it is today. The attributes of good fishing, abundant wildlife and berries attracted Native People to Basswood Lake and there is archaeological evidence for at least 9,000 years of use of the lake. These same attributes also attracted tourists to the area. A 45 lb 9 oz Northern Pike was caught on Basswood Lake in 1929 and this remains the Minnesota state record. There is good northern pike, smallmouth bass and walleye fishing virtually everywhere on Basswood and lake trout thrive in the cold, clear deep waters of most of the Canadian side of the lake, with Bayley Bay and North Bay being especially renown trout waters. The shallow water sections, located primarily in the southern part of the lake, are home to bluegills and crappies. The attraction of Basswood Lake, undoubtedly one of the most productive and diverse lakes in the entire Boundary Waters region, continues to this day.

The lake was a busy tourist area and there were twenty resorts operating on Basswood Lake in 1942. Some were small resorts that catered to families and provided opportunities for fishing, canoeing, swimming and relaxation, while others primarily catered to fisherman. A few, such as Basswood Lodge, were family resorts that featured luxurious dining on gourmet foods in addition to hot showers and flush toilets. During the day, guests were fishing on the lake, primarily in motorboats, or remained at the resorts to swim or simply relax. In addition to the resorts, houseboats were also present on the lake. Although the lake was busy during the day, people returned to the lodges for the night and campsites were used less than they are now. Although motorboats were more common on the lake than canoes during the resort years on Basswood, people were also or using canoes at the resorts and going on canoe trips.

Although most people and supplies got to Basswood Lake via the motorized Four Mile Portage, some arrived by air. Ely was the hub for float planes flying to resorts in the area as well as flying fishermen and canoeists to their destinations. Ely was the largest inland seaplane base in North America in 1946. In 1949, height restrictions for flying over the BWCAW were put in place. The restrictions on flying, and other restrictions, led to a demise of the resorts. This was a period of intense debate, acrimonious charges and numerous court battles between those favoring motor use and wilderness advocates. Many decades have passed, the debates continue and the wounds have still not completely healed.

In contrast to today, logging was occurring on Basswood in the 1940’s. Logging was being carried out on the Canadian side of Basswood Lake, with newly initiated 300 foot shoreline restrictions, in 1942 and 1943. J. M. Matheiu had two logging camps on Basswood Lake, one on Sunday Bay and another on Canadian Point.

Logging on the American side of Basswood began in 1895. Accessible lumber declined in the early 1920’s and the two large mills in Winton, Minnesota that were the destination for much of the lumber, Swallow and Hopkins and St. Croix, closed in 1922 and 1923. Logging continued near Basswood Lake at a slower pace in the 1930’s. Frank Hubachek bought land on shore of Basswood when he heard that large pines along the shore were scheduled for logging in 1937. This became the site of the Basswood Wilderness Research station.

Bob’s Work History in Quetico Park

Bob on Agnes Lake in Quetico Park

Bob on Agnes Lake in Quetico Park

Bob saw a lot of Quetico Park in the relatively short time he worked there. As mentioned previously, in addition to working out of the Bayley Bay and Cabin 16 ranger stations on Basswood Lake, he also worked on Beaverhouse, Lac La Croix, and Pickerel Lake. Gerry Payne, his partner on Pickerel Lake, told Shan Walshe that Bob Hayes was “the best partner a fellow could ask for because he was easy to get along with and could handle himself in the bush.”

Bob guided for twenty-one years and for fourteen years he was head guide for the Trail Riders, a group associated with the American Forestry Association. He did all his guiding in Quetico Park. On his trips, the emphasis was on traveling and seeing as much of Quetico Park as possible. Fishing was an important part of the trip, but they fished mainly for food. They would stop when they had enough for a meal of fresh fish. Bob told his clients that he wasn’t mad at the fish and they wouldn’t keep catching fish they didn’t need.

Conversing around the campfire was an important part of the trip. Bob is a good storyteller with lots of canoeing and camping experiences to relate. When a young guide asked him for advice on guiding, Bob told him, somewhat in jest, to “take lots of whiskey”. In the spirit of Bill Magie, Bob Cary, Sigurd Olson and other north woods guides, many stories were told around the campfire. I’m sure that many people ended their trips with Bob with stories, not only of their own exploits, but also tales that they heard from Bob Hayes.

His favourite starting point for a trip was Powell Lake. They would fly to Powell Lake and come down Clay Creek, now called Greenwood Creek, and the Wawiag River to Kawnipi Lake. Lower water levels and warmer temperatures in recent years have made Greenwood Creek paddleable only in the spring. From Kawa Bay of Kawnipi there are numerous routes to take back to Moose Lake or Fall Lake. Some of his other favourite spots in Quetico are McEwen, McIntyre and Robinson Lakes. Bob would pick a route that best suited his clients’ interests and experience.

Recent Years

Bob and Leone Hayes

Bob and Leone Hayes

Bob and Leone have known each other for over sixty-four years and have been married for fifty-eight years. It all began on Basswood Lake and they have maintained their interest in Basswood Lake and Quetico Park. In a letter to the Atikokan Progress and the Fort Francis Times regarding the possible closure of the southern entry stations to Quetico Park. Bob wrote “the BWCAW is a magnificent area but somehow it lacks the magic of Quetico. In my opinion, the Quetico is the finest piece of ground and water on the planet.”

They live in Winton, Minnesota, just a short distance from where they met on Basswood Lake. They have often returned to camp on Basswood Lake – first by themselves, then with children and finally with grandchildren. They have remained active and when Leone’s daughter and daughter-in-law go for walks with Leone they both mention that have a hard time keeping up to her. Bob has had knee surgery, or he, also, would also be hard to keep up with. Leone is also known throughout Winton for taking her homemade soup to people who aren’t feeling well.

Bob says that he “left the employ of the Ontario Department of Lands and Forests to marry a woman I couldn’t live without – I still can’t.” The pair that Shan Walshe called ” the nicest couple I know” are thriving in their home not far from where they met on Basswood Lake.

Robinsons of Souris River Canoes

Here’s to You, Mr. and Mrs. Robinson

Most people come to Atikokan, Ontario to paddle canoes; the Robinson’s, however, came to Atikokan to build them. They also happily put their own canoes to use by paddling the numerous lakes, rivers and creeks that are found on this portion of the Canadian shield. Atikokan is justifiably known as “Canoeing Capitol of Canada”. In addition to Quetico Park, it has the White Otter Wilderness area to the north and numerous lakes and river systems accessible by logging road or by float plane.

Keith and Arlene Robinson started the Souris River Canoe Company along the banks of the Souris River in southern Manitoba in 1985. The Souris River is thought to be based on a Sioux name that means “foaming river” because of the foam that forms below small rapids and rocks. The early French explorers and traders translated “foaming river” into French and called it the Mousse River because “mousse” means “foam” in French. Then, in an example of multicultural miscommunication, English speakers evidently simply changed Mousse River into Mouse River. In the final twist in this tale of the mouse, later French immigrants then converted the Mouse River into Souris River. “Souris” means “mouse” in French and it may have been called Mouse River because it is a narrow river that twists and turns like the tail of a mouse as it meanders through the prairies of Saskatchewan, North Dakota and Manitoba.

Some people, including the Robinson’s, prefer a different explanation of the name. “Missouri” means “large canoe” in one of the Sioux dialects and “souri” means “small canoe”. They named their company Souris River Canoes since they were making canoes in Souris, Manitoba, along the banks of the Souris River. The recreational canoes they built were “small canoes” compared to the voyageur and other trade canoes that traveled down the Souris River in the 1700’s and 1800’s.

Prior to building canoes, Keith and Arlene lived in Snow Lake Manitoba. Keith worked as an environmental scientist at a copper-zinc mine and Arlene taught music in the high school. During this time they both did a lot of canoeing on the numerous lakes that surround Snow Lake. They honeymooned on the Grassy River south of Snow Lake and continued to use canoes to explore the rivers and lakes that surrounded them in northern Manitoba. They got involved in marathon canoe racing in the early 1980’s. While racing, they got to know Everett Crozier, a canoe builder from Wisconsin and were inspired to start a canoe business.

With the enthusiasm and brashness of youth, they moved to Souris, Manitoba and started Souris River Canoes. Keith used a mold he obtained from Everett, a man who was also influential in some of the designs of Wenonah canoes, and the first canoes Keith made were based on the designs of Eugene Jenson. Keith decided to incorporate some of his own ideas and began designing his own canoes while in Souris, Manitoba. The market for canoes in Manitoba was limited so he could only sell about thirty-five canoes a year when they were in Souris.

It was almost impossible to break into the United States and southern Ontario markets from Souris, Manitoba so Keith and Arlene decided to look for a location that was closer to the markets for their canoes and that also had other attributes they were looking for. They were hoping to find a small town that had both good canoeing and cross country skiing that would also be a good place to raise a family. Since they wanted to stay in the northern lake country, they began their search in Kenora and Fort Francis and worked their way east. They finally knew they were in the right area when they noticed that there were more vehicles traveling down Highway 11 near Atikokan with canoes on top than there were pulling boat trailers.

Arlene heard about Quetico Park when she was in high school in Souris, Manitoba and she and Keith took their first canoe trip in Quetico in 1991. Started at French Lake with their two young children, Josh and Beth, and paddled into Pickerel Lake. They were amazed at the number and size of the sand beaches on Pickerel Lake, something not common in northern Manitoba. The combination of sand beaches, exposed bedrock, and large trees was very appealing to them. The dynamic crossroads of the northern boreal forest and deciduous forest in a landscape that is almost half water is what makes Pickerel Lake and the rest of the boundary waters area so appealing to the Robinson’s and other outdoor enthusiasts like them.

The Robinson’s moved to Atikokan in 1992 and set up their canoe business in an empty building not far from the Atikokan River. They moved from a town named after a mouse to one named after caribou and they hoped that their canoe business would have a similar growth spurt. Their company has grown in size, but it has remained a family business. They are still working out of the building they bought in 1992.

Wayne Docking, a retired teacher who has worked for Keith for five years, told me that Keith is “dedicated to designing and building the best composite, ultra-light, wilderness tripping canoe in North America.” He learned the basics of making composite canoes from Everett Crozier and has gone on to design the Quetico (in three lengths), the Wilderness 18, and a solo canoe called the Tranquility.

Keith and Arlene canoe with Josh and Beth every summer in Quetico. The entry at Lerome Lake is a favorite of theirs since it takes them into Cirrus Lake, a large, three-section lake with little human activity. It is also gives them access to Quetico Lake, one of their favorite lakes. Quetico Lake with its big, dramatic cliffs, pictographs, sand beaches and rocky, secluded bays is one of the most diverse lakes in Quetico.

Josh and Keith Robinson paddling near Atikokan, Ontario

One of their most memorable trips occurred when their kids were young. They flew into Clay Lake and paddled down Greenwood Creek into Quetico Park. Just as they entered the park, they paddled around one of the many sharp turns in the creek and got a close up look at a large bull moose. The kids, who were only 3 and 5 years old, went wild when they saw the moose. What a wonderful introduction to Quetico! Keith and Arlene had some hair-raising moments going across the bigger lakes Josh and Beth would move around at times when they should have stayed still. Keith said that, on one especially windy day, they were close to tipping. The experience contributed to his grey hair and the experience provided inspiration to design the Quetico canoe.

They zig-zagged through the northeastern part of the park and ended the trip crossing Nym Lake as the full moon was rising on their right as the sun was setting to their left. They were mesmerized by the beautiful, but very different, colours of the moonrise and the sunset on opposite sides of the canoe. The outdoor adventures with their parents has had a lasting effect on their children. Josh and Beth both participated in the Atikokan High School outdoor education program called ‘Outers’ and are active canoeists, hikers and cross country skiers.

Both Keith and Arlene are avid cross country skiers and they felt that the potential for cross country skiing was an important factor in deciding where they were going to re-locate. There were no developed ski trails when they moved to Atikokan in 1992. Arlene was instrumental in starting “Beaten Path Nordic Trails” ski club and was president for a number of years. The club has grown steadily and now has over 100 members and 35 kilometres of groomed trails.

To help with fund-raising for cross country skiing in northwestern Ontario, the Robinson’s have provided canoes for an annual fund raisers for the Thunder Bay National Team Development Centre, an organization that that trains promising, young cross country skiers, and the Kamview Nordic Centre in Thunder Bay. The money raised has been put to good use ñ three former Thunder Bay Development Team cross country skiers participated in the 2006 Olympic Winter Games.

Beaten Paths hosts a race in February called the Chocolate Cup, where all participants get chocolate. Winners also receive a trophy made from chocolate and many skiers undoubtedly eagerly consume their chocolate while recovering from the race. The lure of chocolate and the opportunity to ski the Atikokan trails attracts many people from Thunder Bay and the surrounding area.

The ski club also hosts two events that take place in Quetico Park. Their goal is to get more people to experience Quetico Park in the winter. The Sawmill Lake Tour, which had its inaugural run in January of 2006, covers 24 kilometres and follows old logging roads from the 1960’s and early 1970’s in the northeast corner of the park. This tour is used as a fund-raiser for the Friends of Quetico and skiers who participate in this tour can make donations to the Friends of Quetico.

The biggest event of the year is the Cross Quetico Lakes Tour that was held this year on March 18. The route is from Nym Lake to Batchewaung Lake and then down the length of Pickerel Lake to French Lake. This year will be the fifth annual tour. The long trip, which is on lakes and portages rather than groomed trails, has had participants ranging in age from ten to seventy. The tour starts at 7:00 a.m. and the goal is to finish by 4:30 p.m. All four of the Robinsons have completed the tour at least once. Chris Stromberg, who organizes the tour and has been a member of the Quetico Park Portage Crew for the last two summers wrote the following about the 2003 trip: “The Cross Quetico Lakes Tour doesn’t include numbered bibs or stop watches. It is a group tour that brings you back to the roots of cross country skiing, across frozen lakes and portages. I can’t think of a better place to hold the event than Quetico Provincial Park. It is a tough tour of 35 or 45 kilometres but skiers have an entire day to finish it. It is by no means a race and there are even a couple of rest stops along the way inviting people to relax around a fire, with coffee provided.”

Keith and Arlene have been active in The Friends of Quetico and Keith served as the chairman from 1998 to 2003. Keith’s main accomplishment while serving as chair was the publication of “Quetico Provincial Park: An Illustrated History” by Shirley Peruniak. Although Keith is no longer chairman, he continues to make important contributions. The current chairman, John Soghighan, told me “Keith leads from any seat at the table with adroit insights, gentle reminders and subtle humor.” It isn’t surprising that Keith and Arlene have been active in the Friends of Quetico during their years in Atikokan since Quetico Park was the biggest factor in attracting them to the area.

The Robinsons have demonstrated a keen interest in the future of the boundary waters area that goes far beyond making canoes. Robin Reilly, the Quetico Park superintendent, stated that “Keith and Arlene are consistently looking for ways to promote the park and encourage sound environmental management.” With their involvement in environmental concerns and other community activities, they are carrying on the wonderful tradition of many of the entrepreneurs on both sides of the border in the boundary waters area. They are concerned with more than economics and with more than just canoeing. They simply strive to make their communities, and therefore the entire area, a better place to live.

Joe and Vera Meany: 26 Years in Quetico

Vera and Joe Meany at Lac la Croix Ranger Station in 1978.

Vera and Joe Meany at Lac la Croix Ranger Station in 1978.

Joe and Vera Meany are now retired in their home along a river about 50 km from Atikokan. For 26 years, from 1971 to 1996, they were the Quetico Park Rangers at the Ranger Station on Lac la Croix. During their years in Quetico, the Meanys built a strong reputation as extremely competent and helpful Park Rangers. In addition to selling park permits and fishing licenses, they also enthusiastically carried out other tasks associated with their job. These included rescuing people who had swamped their canoes and removing innumerable fishhooks embedded in fingers, Joe and Vera Meany at Lac La Croix Ranger Stationlegs, and other, more tender parts of the anatomy. Joe removed so many fishhooks that he was known around Lac la Croix as “Dr. Hook.”

Their many summers in Quetico aided them in advising canoeists about the rapids on the nearby Maligne River and other areas where problems can be encountered. They were also reliable sources of information on fishing, wildlife, pictographs and campsites. One of the real benefits of having Ranger Stations on the edge of Quetico, with knowledgeable people like Joe and Vera manning them, is the opportunity it gives canoeists to find out the current conditions of portages, the places where bears are causing problems, and other up-to-date and accurate information.

A canoe trip into Quetico can be a daunting adventure, especially for novice canoeists. Through their efforts, the Meanys made Quetico canoe trips a safer and more enjoyable experience for thousands of people. Because of the assistance they gave to Boy Scouts from Omaha, Nebraska and other Nebraska canoeists, they were made honourary citizens of Omaha, Nebraska by the town’s mayor.

Joe took a round-about route to Quetico Park. He grew up in Kirkland Lake, Ontario and started working as a diamond driller when he was fourteen. He celebrated his fifteenth birthday working in Pickle Crow and worked in underground mines in Kirkland Lake until he was old enough to join the army. He served 5 years in the army, including eighteen months in Korea.

Vera grew up on Prince Edward Island and later moved to Toronto where she worked with Joe’s sister. She and Joe were married in 1955 and in 1960 they moved to Atikokan where Joe worked in the iron ore mine. Since arriving in Atikokan, their lives have revolved around canoeing. Joe became one of Canada’s top canoe racers and in 1963 teamed with former Atikokanite, Eugene Tetreault, to win the Canadian Professional Championships. Joe won it again the following year with his brother, Don Meany. Don, also an Atikokan resident, now makes bent-shaft canoe paddles with his son, Spencer, that many consider to be among the best in the world.

To help mark Canada’s centennial in 1967, Joe was part of a three-man crew that paddled a kayak from Edmonton to Montreal in forty days. The race, however, that still puts a glint in his eye and animation in his body is the 1964 Atikokan to Ely race. In 1964, Joe and Eugene Tetreault won the marathon race from Ely, Minnesota to Atikokan, and after a days rest, back to Ely. This race, which passed through the centre of Quetico Park, was one of the premier canoe races in the 1960’s. Ralph Sawyer called it the “ultimate canoe race” because it required day and night paddling, crossing a wilderness of lakes and rivers, and had numerous portages.

In 1964, the race involved paddling from Shagawa Lake in Ely to Atikokan, resting a day in Atikokan, and then returning to Ely. Racers could take any route they wanted but there was a route that virtually everyone used because it was believed to be the fastest route. Joe and Eugene, however, decided to shorten the normal route by cutting portages through a low, boggy area between Alice and Fern Lake. A combination of terrific paddling and their shorter but more difficult route brought Tetrault and Meany the victory in the 1964 race.

The legacy of that race lives on in Quetico. The southern portage they cut was named “Bonne Homme” Portage (French for “good man”) after Eugene Tetrault. The northern portage that leads to Fern Lake was named “Sauvage Portage” after Joe Meany. It was originally named “Maux Jit Sauvage” but it was shortened to “Sauvage Portage”. Unfortunately, only the name was changed, the portage remains as long as ever. Both portages are difficult to find, very long, bug-infested, and are knee deep in mud in places. There is a joy, however, in completing them and they do connect two beautiful lakes with seldom visited, scenic, small lakes between the two portages.

Joe has never lost his desire to paddle long distance, and in 1985 he kayaked with his friend Keith Burand around the southern half of Quetico. They paddled non-stop for 34 hours to cover the 200 kilometres and 27 portages. The legacy of Joe’s racing days is still evident in the paddling style of the portage crew who work in Quetico. The Quetico Park portage crew use the “hut stroke”. They steer by switching sides instead of using the j-stroke and, consequently, all their effort goes into forward motion. Many paddlers in Quetico recognize the portage crew from a distance because of their distinctive, efficient paddling style. Joe’s love of canoeing, love of Quetico, and his job as a Quetico Park Ranger were a perfect match.

Vera was always the main office worker, she kept the office running smoothly and efficiently. She also played a central role in helping others, my wife and I included, in dealing with the complexities of running a Ranger Station. She and Joe also raised two sons, and one former portage crew member told me that “Vera became a second mother to me”. A whole generation of young men and women working in Quetico as volunteers, Junior Rangers and portage crew describe Vera as their surrogate mother during their summers in the park. Providing meals for portage crew, volunteers, Junior Rangers and canoeists who happened to stop by when meals were being served, goes well beyond the job description for park station attendants. Vera, however, was always generous with her time, her advice and her food.

Vera was also renowned for her home remedies for a wide variety of ailments. These came in especially handy when a child living at a ranger station got sick and a doctor, or even medical advice, was hard to come by. Over the summers the Meanys were at Lac la Croix, Quetico Rangers got recipes for cough syrup made from onion juice, a cream for rash made from corn starch and lard, and a remedy for canker sores. One summer when we were at the Beaverhouse Ranger Station, we ran out of shampoo and Vera called us with a recipe for shampoo made out of mayonnaise, lemon juice, and dish detergent.

Joe and Vera made numerous improvements to the Lac la Croix Ranger Station and the surrounding structures. Their main addition was a log building made from red pine logs that Joe obtained from a variety of locations on Lac la Croix. Joe got permission to build a woodshed from park authorities and he then proceeded to build a log building with an attached woodshed. During the time Joe and Vera were at Lac la Croix, it was known as “Ranger Hall”. It functioned as a museum complete with a large number of photos and articles relevant to the history of the park.

Many canoeists made a point of seeing the Meany’s at Lac la Croix every summer. If they didn’t start or end their trip at Lac la Croix, they planned their trip with a stop to see the Meany’s as part of their itinerary. At Cache Bay and Prairie Portage Ranger Stations we periodically met people who were paddling long distances across Canada. It always seemed that they had either just had an extended visit with Joe and Vera or were on their way to see them because someone along the route had told them that the Rangers at Lac la Croix were people they “absolutely” had to see to make their trip complete.

Vera and Joe always had a large, well-used coffee pot and over the years many canoeists had a hot cup of coffee while describing aspects of their canoe trip while waiting for a towboat or a flight back to Crane lake. Joe and Vera especially enjoyed talking to people at the end of their trips when the days and nights in the park have mellowed people and made them eager to share their experiences. As to the multitudes of cups of coffee that have been consumed, Joe said that he had found that “when you give a cup, you get a pot back”.

When I talked to Joe and Vera the year before they retired, they wrote back and stated, “We take each year as it comes now, each year brings us closer to the time when we will have to leave the Lac la Croix station where we have spent so many memorable summers and have met so many wonderful people from around the world. It is our hope that after we leave the coffee pot will always be on, and the lamp in the window will remain lit for the inconvenienced visitor. We will miss the Ontario Ranger girls, the portage crew paddling in doing the “hut stroke” and the tow boats and aircraft bringing in new and old visitors to Quetico. But that time is not quite yet.”

Vera and Joe Meany at their house near Atikokan in July, 2006.

In 1996, their reign at the Lac la Croix Ranger station came to an end. The Meanys became part of the fabric of Quetico during their twenty four years at Lac la Croix. They are part of the Park Ranger tradition that includes people such as Bill Darby, Ted Dettbarn, Lloyd Rawn, Art Madsen, Bob and Evelyn Halliday, Mike and Priscilla O’Brien, Webb and Berniece Hyatt, and numerous others. The Quetico wilderness is indeed composed of men and women that are a match for the magnificent landscape they inhabit.

Devil’s Crater – Portal to the Past

By Jon Nelson & Leif Nelson

crater_canyonMy first glimpse of Devil’s Crater took my breath away. I was shooting aerial photographs of outpost cabins for a local outfitter when the pilot and I decided to take a detour to look at an unusually shaped lake off in the distance. In a few minutes, the small, almost perfectly circular lake was below us. Surrounded by towering cliffs, it lay in the midst of a gently undulating topography filled with the bogs, creeks, small lakes and boreal forest that are typical of northwestern Ontario. In an otherwise relatively flat landscape, the crater’s presence, along with the kilometre-long canyon just southeast of it, was a mystery.

I knew immediately that I had to see this remarkable formation up close. My son Leif, a graduate student at the University of Waterloo, and my good friend Al Maddox, a retired teacher and experienced canoeist, were eager to accompany me. Devil’s Crater is located some 150 kilometres north of Thunder Bay, Ontario. There are no roads within 20kilometres of the crater and canyon, so we had Huron Air from Armstrong, Ontario fly us in. We landed on a small lake connected to the canyon via a narrow creek.

In the last days of June, we found ourselves crowded into a single canoe, heading down the creek toward the crater. Before long, however, a combination of shallow water and boulders made further progress impossible. Despite much searching, we could not find a portage, although we knew that two other groups from Thunder Bay had reached the crater by this route during the last few years. In 1997, Bill Ostrum, the owner-operator of a Thunder Bay company that designs and makes packs, had paddled to the small lake we had landed on and attempted to walk to the crater along the side of the canyon.Travel was very difficult, because a forest fire in the 1980’s resulted in dense growth of jack pine and a lot of blowdown, and he turned back. Julian Holenstein, an Environmental Consultant for the city of Thunder Bay, Ontario, was told about the crater by Bill Ostrum and the following summer, he led a group of four people to the crater. The next summer, Bill and Anne Ostrum also reached the crater. These two groups, and undoubtedly others, had reached Devil’s Crater by the same general route that we were now using.We couldn’t, however, find any evidence of the portage that they used to bypass the unpaddleable section of the creek so we quickly put in a “minimalist” portage that was roughly parallel to the creek and avoided wet areas and large rocks. If this route gets used very much the portage will undoubtedly be rerouted somewhat but it served well for our purposes.

In addition to the summer excursions, Volker Kromm, a forester with Abitibi Consolidated, and two companions made a trip by snowshoes into the crater in the winter of 2003-2004 to do some ice climbing. They successfully climbed both waterfalls that enter into the crater and took core samples of red pine, growing near their northern limit, that grow along the edge of the crater.

In addition, Native People have undoubtedly visited Devil’s Crater numerous times over thousands of years. Although the canyon and crater wouldn’t have had much appeal for hunting or fishing, a site this unusual has an appeal that goes beyond just obtaining resources.The crater is also part of a trapline for a member of the Gull Bay First Nation on Lake Nipigon and First Nations communities in the area have a long history of visiting the crater.

canyon_from_canoe-2We had a beautiful paddle up the canyon. The day was cool and sunny, and there was enough wind to keep the bugs to a minimum. Along the canyon shoreline were large rocks and scree slopes at the base of the cliffs. In other spots, the majestic cliffs soared directly out of the dark waters, in which we could see the shimmering reflections of our surroundings.

A study of the vegetation in the nearby Ottertooth Conservation Reserve was conducted by Al Harris and Robert Foster. They found that the large forest fire in 1980 resulted in a landscape dominated by young jack pine mixed with trembling aspen and white birch. There are also isolated small stands of red and white pine, both of which are near the northern edge of their range.Some old stands of black spruce and cedar are found in the swamps. On the west-facing cliffs along some of the lakes they found three arctic alpine plants, Nahanni oak fern, smooth woodsia and showy locoweed, that are rare plant species in Ontario. North facing cliffs at Ottertooth Canyon support an exceptionally rich community of arctic alpine plants including Snowy Arnica, Appalachian Firmoss, Northern Woodsia and Northern Goldenrod. Although no botanical surveys have yet been completed at Devil’s Crater, its similar cliffs probably also provide habitat for some interesting species.

We were eager to fish as we had heard that brook trout might be present. We fished for a short time as we paddled up the canyon and managed to catch a northern pike but no trout. I found that, as gorgeous as the canyon was, it was difficult not to keep looking ahead trying to catch a glimpse of our destination: Devil’s Crater.

The only obstacles we encountered while paddling up the canyon towards the crater were a two-metre high rock wall that we had to portage over near the beginning of the canyon and a short section near the end of the canyon closest to the crater where it became too shallow to paddle the canoe.We then paddled across a large pool which marks the end of the canyon.

A large amount of scree coming down from both sides of the canyon forms a plug across the narrow opening between the canyon and the crater. We made our campsite along the edge of a grassy area through which the narrow creek coming out of the crater meanders. Our spot was small and uneven; nevertheless we pitched our tent on one of the few dry openings in preparation for a two-night stay. (**We found out after our trip that camping is not permitted in some of the Nature Reserves. There isn’t, or at least wasn’t at the time of our trip, notice of a camping restriction for Pantagruel Creek Nature Reserve on the Ontario Parks website. However, to be on the safe side, contact the Park Superintendent before entering an Ontario Park.)

We were hoping to portage along the base of the scree and reach the crater with relative ease. As the designated photographer, I went ahead and climbed partway up the side of the crater. Leif and Al had the much harder task of hauling the canoe over a great jumble of boulders while weaving it through trees and shrubs – so much for the “relative ease” plan. From my perch I could see two small waterfalls cascading down the cliffs that formed the far wall of the crater – the only visible sources of water entering Devil’s Crater.

Devil's-Crater

devils_crater_canoe

crater-waterfallDespite what the lake’s name would suggest, a meteorite did not create Devil’s Crater. The impressive force responsible for the crater’s creation, and the canyon stretching out below it, was the combination of the retreat of the Laurentide Ice Sheet and the overflow of glacial meltwater from Lake Agassiz, which was then located just west of the crater. The flow from the two small waterfalls that now enter the canyon is a mere fraction of the torrent that carved this feature into the landscape over 9,000 years ago. Thousands of years of erosion have also softened the crater and canyon. Falling rock combined with lichen growth make it difficult to determine just how much water must have surged through the kilometer-long canyon when Lake Agassiz overflowed. The events that produced Devil’s Crater not only altered the landscape significantly, but may well have been the catalyst for climate change and influenced the migratory patterns of the first humans who lived in this area.

Approximately 18,000 years ago, the air temperatures of the earth began to rise as the planet emerged from the most recent Ice Age. Massive continental glaciers, including the Laurentide Ice Sheet that had blanketed most of central North America were slowly retreating. The water pouring out from the melting Laurentide Ice Sheet – which covered much of what is now Ontario, Manitoba and parts of Quebec, Saskatchewan, Nunavut, Minnesota and North Dakota – produced enormous lakes. One such lake was Lake Agassiz, which was formed to the south of the retreating glacier. Lake Agassiz extended over more than 1.5 million square kilometers, an area larger than all the present Great Lakes combined. As the lake slowly shifted northward following the retreat of the massive glacier, its shape, size and position changed significantly. Over a 5,000 year period, various outlets routed the lake water in three different directions: south through what is now the Mississippi River Valley to the Gulf of Mexico, east through the Great Lakes and what is now the St. Lawrence River to the Atlantic Ocean, and finally north to Hudson Bay and the Arctic Ocean.

Changes in the direction of the outflow of Lake Agassiz would have significant consequences. It has been generally accepted that the eastern overflow of Lake Agassiz initiated some 11,000 years ago resulted in a tremendous amount of glacial melt-water surging through the Great Lakes basins into the North Atlantic Ocean. The influx of fresh water essentially diverted ocean currents in the North Atlantic, resulting in a significant cooling of the climate in North America and Europe.This 1000-year cooling period, referred to as the Younger Dryas, is characterized by the lowering of average air temperatures around the North Atlantic at a time when global temperatures were increasing.

Phil Kor, the Senior Conservation Geologist for Ontario Parks who has researched this topic, says, “Although recent research is challenging this theory, as alternate routing of the meltwater from glacial Lake Agassiz is being considered, the influx of an enormous volume of fresh water into the North Atlantic from the Great Lakes basins still seems to be the best explanation for changing ocean currents and the climate in North America and northern Europe.”

As Lake Agassiz continued its northward shift, the land behind it slowly rebounded as the great weight of the glacier withdrew. Water from Lake Agassiz flowed south when ice occupied the Superior Basin. Then it flowed again to the east, this time through Lake Nipigon and on to Lake Superior and the North Atlantic Ocean. Large volumes of water flowed through channels that today are shallow streams and creeks.

devils-crater-from-airplaneAs the glacier receded, new outlets formed in a northerly pattern. The water ran through this new area with such tremendous force that it carved Devil’s Crater, along with the canyon southeast of it, out of the bedrock of the Canadian Shield. In creating this deep gash in the landscape, the rushing water worked in tandem with local geology. The crater and the canyon probably began as a fault in the bedrock. The immense overflow eroded the bedrock along the fault to create the crater and the canyon.

Eventually, the continued retreat of the glacier and the rebounding land surface behind it opened up new outlets north of Devil’s Crater. The outflow through Devil’s Crater would have lasted only a short time, anywhere from a few years to a couple of hundred years. James Teller, professor of geology at the University of Manitoba and a leading researcher on Lake Agassiz overflows, describes the crater as “a paleoplunge basin, formed by Lake Agassiz overflow that eroded the less resistant diabase on the down-flow side of the fault contact with the resistant granite”. Devil’s Crater is a dramatic example of what moving water can accomplish in a relatively short period of time.

From inside the crater, the view is incredible. Two-thirds of the crater’s edge is a curved wall of dramatic, lichen-encrusted cliffs that rise more than 70 meters directly out of the water. When seen from a canoe on the lake, the cliff walls seem even higher because the lake is only about 200 metres in diameter. The remaining portion of the crater’s edge is a steep slope composed primarily of large boulders. Al noted that, from some locations, there didn’t seem to be any way out other than scaling the cliffs. Near the middle of the lake, we tied a rock on the end of a rope and lowered it to the bottom in an attempt to estimate the depth of the water. We were astounded to find that our primitive measuring device indicated that this tiny lake is approximately 70 metres deep.

When traveling into and out of the crater, we were paddling near the bottom of a spillway formed more than 9,000 years ago. What is now a canyon was once filled with water that moved with enough force to enlarge a crack in the bedrock and form a chasm. The area we traversed on our way into the crater, which is now a mass of car-sized boulders, was once submerged beneath at least 50 metres of rushing water. Today, large white and red pine trees grow along the canyon and near the edge of Devil’s Crater.

Researchers, primarily Dr. James Teller and associates at the University of Manitoba have found that the terrific amount of water that once tore through this area left behind remnants of riverbeds, broad, flat deposits of sand and gravel, and giant boulders at various locations between Lake Agassiz and Lake Nipigon. In recognition of the significance of these area, the Pantagruel Creek Provincial Nature Reserve and the Ottertooth Conservation Reserve where created. Ottertooth Canyon, Devil’s Crater and Mink Bridge Portage Falls on the Kopka River were all created by glacial melt water surging out of Lake Agassiz towards the Lake Nipigon basin and on towards the Atlantic Ocean.Bill Ostrom has noted that probably nowhere else in Ontario are there three such spectacular landforms so close together.

Lichens, herbs, grasses and shrubs quickly populated the newly exposed land. Large, cold-adapted grazing animals such as woolly mammoths, muskox and barren-ground caribou thrived. So did sabretoothed tigers and “dire” wolves, which grew to one and a half times the size of timber wolves. The most intimidating predator of all, human beings, may also have been present. Palaeoindians, the first people known to have inhabited this region, probably followed the large mammals in their northerly migration.

However, by the time Lake Agassiz overflowed into Devil’s Crater, the woolly mammoths, sabretoothed tigers and dire wolves were extinct, but caribou continued to be a main source of food for Palaeoindians. In 1957, a caribou antler recovered from the bottom of Steep Rock Lake near Atikokan, Ontario, was determined, through carbon dating, to be nearly 10,000 years old. William Ross, a retired regional archaeologist for the Ministry of Tourism, Culture and Recreation for the Thunder Bay region who is generally regarded as a leading authority on the archaeology of northwestern Ontario, told us that “There is a strong possibility that Palaeoindians were witnesses to the dramatic overflow of Lake Agassiz. The water surging down the east side of Lake Agassiz may have prevented these early peoples from expanding northward until the waters subsided enough that a crossing to the north could be safely made.”

Floating in our canoe on the small, placid lake inside the crater, we were in awe of what occurred here at the end of the last Ice Age. The crater’s two small waterfalls are reminders that just over 9,000 years ago, an outpouring of water draining a lake that stretched all the way to Saskatchewan careened and swirled through here with devastating power to form Devil’s Crater and the canyon below it. These formations are portals to the past. They remind us how, in an instant of geological time, a piece of Ontario’s terrain was dramatically altered.

Leif Nelson was a graduate student in the Earth Sciences Department at the University of Waterloo when this article was written. He now works for the Ontario Ministry of the Environment.

Life Under the Ice

During the winter, all life under the ice has to adapt to conditions that are strikingly different from those found in the summer. In the summer, our lakes are layered with the warmest water on top and the coldest on the bottom. As you descend, the temperature slowly decreases until you reach the thermocline where there is a sharp drop in temperature. This invisible line separates the more productive waters that contain microscopic plants called phytoplankton from the much colder, darker areas below.

Ice on a Northern Ontario lake.

ice_on_northern_lakeThe thermocline is just below the surface in the spring and fall and drops to twenty-five feet or more in midsummer. Lake trout, burbot and a few other species of fish spend almost all their time below the thermocline and just enter the warmer waters for short periods to feed. They move up and down depending on the thermocline and even come to the surface when the temperature of the lake water is the same everywhere in late fall and early spring.

In winter, the water beneath the ice is also layered, but it is the opposite of what is found in the summer. This, and the unusual properties of ice, is due to the bizarre chemistry of water. Water is the most dense at 39 Fahrenheit (4 Celsius) and consequently the water at the bottom of deep lakes is this temperature regardless of the season. This causes a topsy-turvey world where the warmest water in the winter is on the bottom (39 F.) and the coldest water is just below the ice (32 F.) at the top. Consequently, a lake trout swimming at a depth of 80 feet in the summer is in the coldest water in the lake and the same lake trout swimming at the same depth in winter is still at the same 39 temperature but is now in the warmest water in the lake.

Anyone who has forgotten to add sufficient antifreeze to a vehicle or didn’t drain the plumbing at their cabin is well aware that ice expands as it freezes. Water is highly unusual in expanding, rather than contracting, as it goes from a liquid to a solid. If it acted like most compounds, ice would sink as it formed, and ice would be continuously forming at the surface and dropping to the bottom. This would cause lakes to freeze from the bottom up. Much ice would form and sink to the bottom on a -35 night in January.

Virtually all our lakes, with the possible exception of the deepest, largest lakes, would be solid ice by March. This would obviously be devastating to life in our lakes. Since ice forms on the top of the water, it puts an insulating layer between the water and the colder air above. This greatly slows the formation of more ice. The accumulation of snow on top of the ice adds another, and better, insulating layer. Even with these insulating layers, we can still get over three feet of ice. This is a strong testimony to the severity and length of our winters.

Ice and snow protect from the cold, but they also greatly decrease the amount of light entering the water. The combination of low light levels and low temperatures causes photosynthesis to virtually stop in the winter. Phytoplankton levels drop dramatically and, therefore, the production of oxygen virtually comes to a halt. The amount of oxygen that is in the water at freeze-up has to last until the ice-cover melts in the spring.

Fortunately, the colder water is, the more oxygen it holds. Once again the chemistry of water works to the advantage of living things. Water obtains oxygen from two main sources: the photosynthetic organisms growing in it (phytoplankton, algae and photosynthetic bacteria), and from direct contact with the air. Both contact with the air and light levels are dramatically reduced at freeze-up and consequently very little oxygen is added to water during the winter. This means that for almost half the year, fish and other oxygen-using organisms, have to get by on the oxygen present when the ice forms.

Since photosynthesis virtually stops, no more food is being made and the amount of food under the ice dwindles during the winter. It’s no wonder that many organisms cope with these conditions by slowing their metabolism. Cold-blooded reptiles and amphibians that overwinter under the ice survive by hibernating in the mud at the bottom of ponds or shallow bays of lakes. A frog meet its oxygen requirements by simply breathing through its skin. The skin’s large surface area allows it to remain stationary and still take up enough oxygen so it can survive a sleep of half the year.

Turtles meet their oxygen needs in a different way. They are also found at the bottom of shallow bays or ponds, but take in oxygen through their cloaca, the opening to their reproductive and excretory systems. They can do this because it is lined with a rich network of blood vessels that functions as a gill. Since lungs are specialized organs for breathing air, organisms like frogs and turtles have adapted other ways of absorbing oxygen from water.

Many microscopic organisms, such protozoa and rotifers, form protective shells known as cysts and remain in an inactive state until the water warms up in the spring. Water fleas and other small crustaceans produce thick walled eggs in late autumn and these survive through the winter and hatch in the spring.

Many fish also slow their metabolism in the winter. Species that spend most of the time in the warmer parts of the lake in the summer, such as largemouth bass, smallmouth bass, and walleyes, become much less active in colder water. This significantly lowers their requirements for both food and oxygen. They won’t increase their activity until the water warms in the spring.

Fish that spend most of the summer in the cold water below the thermocline continue to be active throughout the winter. Lake trout are the best-known species of fish that stays active all winter. They thrive in cold water and travel freely throughout the lake in the winter. Their metabolism remains high and they have to continue to seek out and catch minnows and small fish all winter long. Although the cold does not bother lake trout, the decreasing amounts of both its prey and oxygen levels can be a problem.

It would be interesting to know how lake trout hunt in the depths of the lake where there is little or no light. The deeper you go in the water, the less light penetrates. Even in very clear water lakes, light only penetrates to fifty feet or so, and below that it slowly fades to pitch black. Lake trout are caught by people fishing at depths where virtually no light penetrates. Even at shallow depths in winter, they have to capture prey in the very low light that penetrates through the snow and ice. How they accomplish this is one of the many unknowns concerning the winter ecology of our lakes.

Another fascinating cold-water species is the burbot. This unusual looking fish, also known as eelpout or lawyer, is a fresh water relative of the codfish. Burbot have been caught, along with lake trout, in nets at depths of over 400 feet in Lake Superior. They are active all winter and are often caught by people ice-fishing. Their eel-like shape, elongated fins and smooth skin probably account for their being discarded on the ice in spite of their excellent taste.

Whitefish and their smaller relative, ciscoes, are other fish that are active under the ice. Both are usually found below the thermocline in the summer, but often enter warmer water to feed. Ciscoes can be seen surfacing on still days in the summer, but can also be found at more than a hundred feet. Their wide-ranging travels are responsible for their being reported to be important summer food sources for both lake trout and burbot in deep water and loons near the surface.

The conditions faced by organisms beneath the ice is similar in many ways to those faced by organisms at the bottom of the snow pack, in the pukak. The temperatures are constantly just a few degrees from the freezing point, it is either pitch black or with dim, filtered light, and the food source is constantly dwindling. Just like organisms in the pukak, they have met these conditions in diverse and inovative ways.

It is a real challenge for cold blooded animals like fish, reptiles and amphibians to survive the cold conditions under the ice, but there are also a few mammals that enter the water under the ice. A thick coat is obviously needed to survive our winters and animals that enter the water need coats that are waterproof as well as exceptionally warm. Water siphons heat from the body much more rapidly than air and it is extremely difficult for mammals to maintain their body temperature in cold water.

Beavers and muskrats spend most of the winter in their lodges huddled together for warmth. The insides of beaver lodges, insulated with mud and sticks, is many degrees warmer than the outside air. They spend much time grooming and keeping their fur well oiled. They have to enter the water to retrieve food that they have stored in a food cache next to their lodge. Even short immersions in the icy-cold water are enough to put a strain on their systems.

Beaver and muskrat have an unusual metabolic tactic that increases the time that they can spend in the water under the ice. They elevate their body temperature slightly just prior to entering the water and this gives them a few more minutes before their body temperature drops too far. Researchers have also shown that muskrats obtain oxygen from air bubbles trapped under the ice and presumably beavers do the same. Beaver and muskrat also have physiological adaptions that decrease the amount of heat loss when they are in cold water. In their feet and at the base of their tails they have a network of capillaries where the arterial blood flowing toward the extremities passes in close contact with the blood in the veins returning from the extremities. The arteries give up heat to the colder blood returning from the feet and tail. This warms the blood returning to the body and cools the blood going to the extremities. This allows them to maintain a higher core body temperature and their cooler extremeties lose less heat to the water.

Land animals, such as lynx and bobcat, also have a heat exchange system in their feet. This allows them to lose less heat to the cold snow they stand and walk on. They carefully avoid, however, getting their feet wet in the winter. Most other mammals also avoid getting wet, since wet fur loses most of its insulating value. There are exceptions: both mink and otter enter the water in the winter to hunt their prey. When I snowshoe along the French River in the northeast corner of Quetico, I often see otter tracks along the river. Their tracks clearly show that they swim for stretches in the open water and come out and travel along the shore where the river is iced over. I am amazed that an animal can come out of the water in sub-freezing temperatures and travel over land in a wet fur coat. Two special adaptions enable them to do so. They have extremely dense and oily underfur that is both warm and sheds water. They also have outer guard hairs that are hollow for additional insulation, and that interlock with each other to protect the underfur.

Otters have a streamlined body that, with extremely short ears, short legs and heavily furred tail, is also designed to minimize heat loss. Because of their short legs, they have to plow through the snow on land and leave a distinctive trough in their wake. It seems appropriate that this toboggan-shaped animal sides on its belly whenever possible.

The late biologist Olaus Murie, in his interesting and informative book “A Field Guide to Animal Tracks” recalled that he “…was snowshoeing up a small stream when I spied movement in the snowy stream bank up ahead. I realized that it was an otter, and the next moment it slid down the bank. Another one appeared, clambered up the bank and slid down. A third appeared from the hole in the ice, and for several moments I watched these frolicsome animals, climbing, sliding, climbing, sliding, over and over again – until all disappeared under the ice. Their playtime was over, and they all went on their way beneath the ice, as so often they do.”

I have never observed otters playing in the winter but I have seen otter slides in various places in Quetico. There is usually one into the water below the rapids from Quetico to Beaverhouse Lake. Otter slide down the hill adjacent to the portage directly into the fast water that remains ice-free year around.

The docks at both the Canada Customs and the Ranger Station at Prairie Portage were always covered with otter droppings when we arrived in the spring the years we were rangers at Prairie Portage. The open water below the rapids is a prime location for otter to hunt fish and crayfish in the winter. They obviously found the docks a convenient place to come out of the water, bask in the sun and relieve themselves. Beaver and muskrat huddle together for warmth in insulated lodges when they return from the water. Otters, on the other hand, are mainly solitary creatures in the winter and don’t have a primary lodge to return to. They evidently commonly use old beaver lodges for dwellings. They must consume a great deal of food in the winter in order to maintain their active lifestyle and stay warm.

To do this they seek out prey both in open water and under the ice all winter long. They have successfully adapted to our extreme winter conditions both in and out of the water by taking an extremely active and aggressive approach to winter.

Rapids and Waterfalls in Quetico

Silver Falls at end of Saganaga Lake

The high number of rapids and waterfalls in Quetico Park is primarily due to the large amount of exposed bedrock combined with numerous creeks and rivers. Three images of these rapids and waterfalls are shown below.

A Gallery of images of waterfalls and rapids in northwestern Ontario is found in the Photography section. A number of long exposure images of water is found in the “fast water, slowly” Gallery.

Silver Falls is located at the northwest end of Saganagons Lake . Silver Falls is one of the highest and most beautiful falls in Quetico Park and can be most appreciated from along the river below the falls since the view from the portage trail is not very good. Caution should be used when approaching these falls and the portage is found to the right of the falls. The portage, like the vast majority of those in Quetico Park, is thousands of years old and existed long before the arrival of the first Europeans. The water from Cache Bay on Saganaga Lake flows over Silver Falls on its way to Sagonagons Lake. This is the route that leads to the ‘Falls chain’ between Saganagons Lake and Kawnipi Lake.

Falls at Prairie Portage on Basswood Lake

Prairie Portage is located at the east end of Basswood Lake in Quetico Park. This small rapids/falls occurs where the water enters into the east end of Basswood Lake which is located on the southern boundary of Quetico Park. It is strange that this location is called Prairie Portage since there isn’t any indication of prairie anywhere near here today. The name evidently comes from the logging days when horses were kept in cleared fields at this site. The cleared fields have now reverted to forest and Prairie Portage no longer reminds anyone of a prairie. This busy site hasthe Canadian Ranger Station on the Ontario side and the motorized portage for Basswood Lake on the Minnesota side.

French River at dusk

This image of the French River was taken at dusk. The French River enters into French Lake near the eastern boundary of Quetico Park. The French Portage, which went from Windigoostigwan Lake to French Lake, by-passed this section of the French River which has numerous rapids. This portage, which parallels what is now Highway 11, is no longer used. There is now a hiking trail which follows along the French River to French Falls. This trail is seldom used and is particularly interesting in the fall and winter.

Falls Road Falls near Thunder Bay, Ontario

Falls Road is a rural road located southwest of Thunder Bay, Ontario. It is apparently named after a small falls that is located adjacent to the road. This photo was taken on a warm, buggy evening in late June. The long exposure, which was over a minute, gives the falls its milky appearance. The overall, blue tint to the image is due to reciprocity failure of the slide film in the long exposure.

Paddling to the McNiece Lake Pines

When I first came to the Boundary Waters I was mainly interested in going canoeing and seeing a new landscape very different from the farm country where I grew up in southern Minnesota. I kept coming back primarily because of the wildlife and it is still thrilling to see moose, wolves, otters, bald eagles, ospreys and loons. I also enjoyed seeing walleyes and lake trout, but I only sought them out when it was time to eat.

My interests expanded as I spent more time in Quetico and other people caused me to see things from a different perspective. Quetico Park has been blessed with many terrific naturalists and I was strongly influenced by Shan Walshe and Shirley Peruniak. They were both working in Quetico when Marie and I started as Park Rangers at Beaverhouse Lake in 1976. Shirley is interested in the human history of Quetico and her enthusiasm and knowledge got me hooked on wanting to learn more about Quetico’s past. Shan Walshe inspired me, along with thousands of other people with whom he came into contact, to want to learn more about plants and their role in the environment. I enjoyed learning how to identify many common plants in Quetico, but I was the most impressed with the trees, especially big, old trees. I remember being shocked to encounter cedars much larger than I thought existed on the Emerald to Plough Portage. It is also interesting to come across trees that seem out of place. The bur oak along Have A Smoke Portage and the silver maples and American elms along the levees of the Wawiag are delightfully eccentric.

Large, mature white pines on McNiece Lake.

It was, however, the sight of an entire lake surrounded by old-growth white and red pines that had the strongest impression on me. I first saw these trees about twenty years ago when I took a trip north of Prairie Portage and last summer I was determined to return to McNiece to see these trees again. That is why I was standing in line at Prairie Portage with my wife, Marie, and our friends Andy and Paula Hill waiting for the Ranger Station to open in the second week of August of last year. I recall working on the inside of that building about twenty years ago and looking out at the line forming well before 8:00. Now they open later so I guess for an August morning we were fortunate in that the line was relatively short. A light very rain was falling and we were eager to be on our way.

The paddle across Bailey Bay was hard since we were quartering into a wind that was gradually increasing. It was a nice break from paddling to do the flat, easy portage to Burke Lake. The rain increased in intensity and I could feel the water slowly wicking its way up my sleeves as I paddled. Prolonged, intense rain always finds a way down your neck and spreads out from there. I figured by the time we stopped to make camp the water moving up my arms should meet the water moving down from my neck.

We stopped for lunch at the end of the portage into North Bay at a nice protected spot where overhead trees kept most of the rain off of us. We were headed to South Lake so we were able to take advantage of the islands to provide some relief from the wind. The paddle through the lilly pads that grow in profusion in the creek leading to South Lake is always a joy. There was just enough water to allow us to keep paddling except in one place where we had to get out and walk the canoes.

One of these years I’m going to spend some time exploring West Lake but once again we just quickly passed through on our way to supper and dry clothes. Afterpaddling a short distance past the portage coming out of West Lake, Marie noticed a pair of small, pink water lilies. Don’t think I’ve ever seen a pink water lily before. We decided to find a campsite on Shade Lake and after much looking we found an unoccupied one. It hadnít stopped raining since we left Prairie Portage, so we weren’t fussy, we simply needed a site with two tent pads. Andy has guided for many years and his expertise in dealing with setting up camp and preparing supper in the rain was appreciated since I have a tendency under adverse conditions to simply eat granola bars and get in the tent. The tarp came in handy and with a fire we were able to dry ourselves and our clothes, eat a hot meal, drink hot coffee and go to bed dry and contented.

The next morning, we woke to the sound of no rain. It was a spectacular morning with blue skies, light winds and cool temperatures. I remember having trouble on a previous trip on the portage from the unnamed lake west of Shade Lake to Grey Lake. It is as confusing now as it was then. There are two beginnings and a confusing intersection about halfway across the portage. If you began on the trail farthest west then you need to take a right at the intersection. Compasses do come in handy sometimes. There are many large white pines on Grey, Armin and Yum Yum Lakes but on Shan Walshe Lake they dominate the forest. As much as Shan loved mature forests and the plants they contain he had an even greater love of wet, boggy places. I hoped that nestled in behind the pines are some interesting swamps and bogs.

The last portage to McNiece passes through large cedars and pines and some of them have very old blazes on them. On McNiece, we were fortunate to find the high rocky campsite that looks west down the lake was unoccupied. We spent two nights at this site and did some fishing and a lot of walking in the woods. After we had set up camp we talked to two people who paddled by looking for a campsite. One of them, Pat Bergman, had worked with Marie at the Outward Bound School in Ely, Minnesota in the late 1960ís.

Mature white pines are the dominant species on McNiece but there are also many mature red pines. It was heartening to see numerous younger white and red pines scattered throughout, including many just a few years old. They were especially prevalent where large trees had fallen and left an opening in the canopy that allowed sunlight to reach the forest floor. White pine seedlings need a lot of sunlight in order to prosper and they are usually out-competed by balsam fir and spruce in shaded areas. Consequently, there are many balsam fir and spruce in the understory and they dominate the understory in many places.

Paula Hill admiring a very large white white pine.

We found white pines up to 3. 5 feet in diameter and there are thousands and thousands of white pine over 2. 5 feet in diameter. We were hoping to find the mother of all white pine but, more importantly, we found a healthy old-growth stand of white and red pine.

The shoreline of McNiece Lake seen through a fog filter at sunrise.

We decided to get up early on the second morning to take photos of pines in the early morning light and were extremely lucky to wake up to thick fog. What a thrill it was to paddle around the lake and take photos of giant pines appearing out of the mist. Hundreds of years ago, much of northern Minnesota and Ontario had pines like this and it was like seeing the past through a fog filter.

We didn’t spend all our time looking at old-growth.  Andy and Paula love to fish,

Andy Hill sitting around an evening campfire.

 which is terrific since all four of us love eating fish. Our days were full and we spent three glorious bug free, August evenings drinking “Quetico cocktails”, watching the sunset and solving the major world problems. It is hard to beat sharing one of the great places in the world with good friends. 

We decided to return to Basswood via Kahshapiwi , Side and Isabella Lakes. At the beginning of the portage out of McNiece Lake  we had the pleasant experience of encountering Scott Wentzell, a son-in-law of Shan Walshe. He and his brothers had started their trip at French Lake and were on their way to Shan Walshe Lake. It was surprising to encounter two groups with people that we know on a lake that is not heavily used.

Two of the portages that we did on our return trip; McNiece to Kahshapiwi and from the bottom of Side Lake southwest to an unnamed lake, made me realize that I, like the pines on McNiece Lake, may have evolved from being mature to being slightly over-mature. The first portage is simply long and has a good hill in to make sure you understand that it is a special portage. The other one must have the most brutal hill in Quetico, or at least that is the way I felt when I finally reached the top. It was good to get back to Prairie Portage, especially after once again crossing Bailey Bay quartering into a strong wind.

Looking back, McNiece Lake seems to be in the centre of a very large stand of old-growth white and red pines since the concentration of these pines increases as you approach the lake and decreases as you move away. Cliff Ahlgren in Lob Trees in the Wilderness states that this is not an illusion and it is what remains of much larger stand of pines. “By 1890, most of the stateís remaining tall pine was limited to the Arrowhead region of northeastern Minnesota, including the border lakes country. The tall pines extended in an irregular band north, east and west of Duluth. On large finger of tall pine reached into the central portion of the present BWCA, with the fingers tip ending in the Quetico, less than ten miles north of Basswood Lake. ” The finger extends a few miles north of McNiece Lake.

The decline in numbers of eastern White Pine over the last two hundred years has been astounding. At the beginning of the 1800’s, white pine was a common, and, in many places, the dominant tree species from Newfoundland in the east to the southeast corner of Manitoba in the west; and from Georgia in the south to the shores of Lake Nipigon in northern Ontario. Dr. William Carmean, professor emeritus of forestry at Lakehead University in Thunder Bay, stated that ìin the early 1800ís, someone could have travelled from the St Lawrence Valley in eastern Canada all the way to the centre of the continent and virtually never been out of sight of magnificent old pines”.

Although the numbers of mature white and red pine have decreased greatly for hundreds of years, they now have many ardent and vocal supporters. The white pine, in particular, has become a symbol of the wilderness in many people’s minds. A forester for the Ministry of Natural Resources in Thunder Bay, Ontario has stated that “to say you are going to cut a white pine these days is about the equivelent of saying you are going to murder your mother. This is not just another species with a problem”.

Numerous studies have shown that mature white and red pines also play significant and diverse ecological roles. A study by the U. S. Forest Service showed that “when female black bears go off in search of food for their cubs, they invariably leave the cubs within a few meters of an old white pine if one is available”. Evidently the deeply fissured bark of a large white pine is the easiest for the cubs to climb if they need to avoid predators. Another study in the Superior National Forest found that approximately 80% of both bald eagles and ospreys build their nests in crowns of old white pines. They obviously seek out these old pines since less than 1% of the mature trees in the Superior National Forest are pines. Even standing dead trees play an important role in the environment. The variety of insects that infest these trees are important sources of food for woodpeckers and other birds. They also serve as nesting sites for a variety of cavity-nesting birds. 

Dead trees, such as this decaying white pine on the north side of McNiece Lake, provide habitats for numerous species of decomposers and the organisms that feed on them.

Researchers investigating the canopies of large trees in the Amazon rain forest and in the mature conifers in Washington, Oregon and British Columbia have found thriving ecological communities in the canopies. They have identified new species of insects, birds, fungus and lichens. It seems inevitable that fascinating discoveries will also be found in the canopies of large stands of old-growth pines in the boreal forest also.

The pines in the McNiece Lake area survived because of their location in an area that the loggers didnít reach before the logging restrictions, and, for some reason, they havenít burned. The logging of white and red pines helped to fuel the economies of the many places, including Minnesota and Ontario, where these pines were common. Both species declined dramatically primarily because of logging but have stayed in decline for many complex reasons that include disease, silvaculture practices and disease. The dead tops on white pines are the “flag” that indicates that white pine blister rust has infected many of the white pines in Quetico and the BWCAW.

Fire can obviously destroy large stands of mature pines but it also is the force that is responsible for the success of white, red, and jack pine forests. Miron Heinselman in The Boundary Waters Wilderness Ecosystem stated that “White pine and red pine can persist without fire for up to 350 and possibly even 400 years for occasional individuals, but without a fire that creates favourable conditions for stand renewal, most stands will eventually be replaced by balsam and spruce as the old pines die.” I couldnít find any records of coring to determine the ages of the pines in the stand around McNiece. We found white pines that were over three and half feet in diameter and there are literally thousands of white pines in the stand that are over three feet in diameter. Based on ages of white pines obtained from coring data, these pines must be well over three hundred years old.

There are many red and white pines in various age classes in the understory around McNiece Lake. There are also, however, many balsam and spruce growing in the shadows of the giant pines. This appears to be a stand that is gradually becoming more diverse as the number of non-pine trees increases. On the other hand, the mature white and red pines seem to be ageing gracefully and many pines, both white and red, are in position to replace them.

It is impossible to predict how much longer the old-growth pines will dominate in the McNiece Lake area. It is a distressing to realize that in the foreseeable future, the magnificent stand of old-growth white and red pines on McNiece Lake will be gone. The trees will not be lost not to the chainsaw or the axe but to the inevitable ravages of time. I remember portaging up a long hill on the northern edge of Mack Lake on the way to Munro Lake in the eastern part of Quetico Park in 1996 and being amazed at how few trees had survived the 1995 fire. The fire raced up the hill through many old-growth white pine burning almost everything in its path. The only trees that were still alive were some of the large, old-growth white pine.

They were blackened and had fire scars along their bases but were still alive because of their thick, fire-resistant bark and branches that remained above the fire. I havenít been back since but these trees probably acted as sources of seeds to the open, nutrient rich ground below. In the past, before fire suppression was so successful, this was how a new pine forest began. William Carmean has written that “old-growth forest management involves more than merely reserving scattered old-growth forest stands. For white and red pine we must also be concerned with regenerating new pine forests, and with the recognition and protection of mid-age pine forests. These newly regenerated areas, and these mid-age forests, thus can become the old-growth forests of the future that will inevitably be naturally harvested by insects, disease and fire.” Fortunately, both Quetico and the BWCAW have stands of middle-aged white and red pines that will be the old-growth for future generations of canoeists.

In retrospect, my reasons for canoeing in Quetico haven’t changed all that much over the decades. I originally came primarily to see large birds and mammals and on the McNiece Lake trip I wanted to see large trees. What is becoming obvious, even to a slow learner like myself, is that what I am really looking for is wildlife in the larger sense: mammals, birds, amphibians, trees, orchids, lichens, and fungi in a natural setting. In Quetico we can find all of this set in a wild landscape of cliffs, waterfalls, pictographs, bogs, creeks, rivers and lakes. No wonder I keep coming back.