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TAKE A WALK ON THE WILD SIDE
Review of:
John Muir 1915. Travels in Alaska. Boston: Houghton Mifflin 326 pp.
[Eighteenth in a series on "naturalist-in" books.]
_________________________________________________________________


John Muir (1838-1914) was born in Scotland and immigrated with his family to the USA

when he was 11.     His early life was marked by hard labour on the family farm in

Wisconsin, under his hard-driving calvinist father.    He was largely self-taught and

showed a genius for inventing and building mechanical devices, including several rather

elaborate wooden clocks.

    Much has been written about Muir and his life, including at least one full-length

biography (Turner 1985). A large part (possibly most) of Muir's published writings are

available at http://www.yosemite.ca.us/john_muir_writings/ .

    Muir was a man of robust health and great physical strength, which served him well

in his wilderness wanderings. He did a great deal of mountain climbing in western

North America, but for him this was not a sport. Rather, he did it to gain a first-hand

acquaintance with the land forms and vegetation of areas that had not yet been

mapped.    And to surround himself with wildness.        The opening sentence of his

autobiographical The Story of my Boyhood and Youth goes to the heart of what he was

all about: "When I was a boy in Scotland, I was fond of everything that was wild, and all

my life I've been growing fonder and fonder of wild places and wild creatures." The

term "creatures" should be understood broadly to include plants, in which Muir was at

least as much interested as he was in animals. His writings show a keen sense of the
2

relationship between plants and habitats.

    Muir was largely self-taught in scientific subjects, but he came to be respected by

the leading natural scientists of his time. He is best known today as a pioneer of the

North-American conservation movement, founder of the Sierra Club, and one who

helped to create the American National Parks Service. He had a special affinity for

California's Sierra Nevada and campaigned for the preservation of some of the most

celebrated natural sites in the USA. His main original contribution to science was in the

area of how glaciers shape landscapes.

    Alaska was acquired by the USA from Russia in 1867. Muir first went there in 1879,

because "To the lover of pure wilderness Alaska is one of the most wonderful countries

in the world." In the trips described in this book, his attention was mainly to the

southeastern part of the territory, especially Wrangell Island and the area around the

Stickeen River on the nearby mainland.       This does not match the popular view of

Alaska. It is a cold-temperate region, a cool rain forest without climatic extremes. It

is far south of the Arctic Circle, and there is no 24-hour daylight in summer. Even so,

the mid-summer sun sets only for a few hours just below the horizon. Another book,

The Cruise of the Corwin, tells of a trip to the farther north.

    Muir had a great deal of contact with native peoples and was even adopted into

one tribe.   However, he has surprisingly little to say about them.       While he was

sympathetic and felt generally at home among them, he seemed not especially

interested in the human element of the region. On the other hand, his Alaska writings

devote much attention to glaciers.       Caribbean people can be forgiven a certain
3

unfamiliarity with glaciers, but in some regions they are such a prominent part of the

landscape that there is at least one field guide devoted to them (Ferguson 1992).

    There are several types of glaciers, but we normally associate the term with valley

glaciers, the type studied by Muir. You can think of these as high rivers of ice, flowing

very slowly down the valley. Ice is constantly breaking off at the lower end, giving rise

to icebergs if this is at the sea.

    Their formation requires quite specific climatic conditions, most particularly high

snowfall in winter, followed by a cool winter, so that much of the winter accumulation

of snow is not lost before the next winter. Over time the snow is compacted into a

mass of ice that flows outward and downward under its own weight. These conditions

are of course mainly found in polar and high alpine regions.

    Although slow, a glacier is a very powerful thing. By its tremendous weight, it

carries and pushes large masses of earth and rock as it advances and can be a major

force in shaping the landscape through which it moves. Fjords, such as those in Norway

and Alaska, are long, narrow coastal valleys with steep sides and rounded bottoms,

originally carved out by glaciers.

    Glaciers are dynamic entities. They constantly change as ice is added in one part

and lost in another.      Furthermore, they grow and shrink in response to climatic

changes. During much of the last ice age, which ended about 11,000 years ago, glaciers

covered almost one-third of the land surface of the planet, versus about one-tenth

today. We are now between ice ages. Even so, eight minor glaciation cycles have been

identified during the past 750,000 years, the most recent from the 17th to the late 19th
4

centuries. In this period, average temperatures were cool enough to permit glaciers to

grow significantly. Since Muir's time, in contrast, they have been in overall retreat

worldwide. Photos of major valley glaciers taken at intervals of decades commonly

show marked changes in size. Even so, at present about three-quarters of the world's

fresh water is bound up in glaciers. Global warming causes a rise in the sea level by

releasing more of this water into the oceans.

     Muir seems to have spent much of his time in Alaska in a state of exaltation. At

one point he remarks that "When sunshine, sifting through the midst of the multitude of

icebergs that fill the fiord and through the jets of radiant spray ever rising from the

tremendous dashing and splashing of the falling and upspringing bergs, the effect is

indescribably glorious."

     And elsewhere: "I reached the top of the highest, when one of the greatest and

most impressively sublime of all the mountain views I have ever enjoyed came full in

sight -- more than three hundred miles of closely packed peaks of the great Coast

Range, sculptured in the boldest manner imaginable, their naked tops and dividing

ridges dark in colour, their sides and the canyons, gorges and valleys between them

loaded with glaciers and snow. From this standpoint I counted upwards of two hundred

glaciers."

     As long as there are truly wild places on Earth, the spirit of John Muir will live

among us.


References
     Ferguson, S.A. 1992. Glaciers of North America: A Field Guide. Golden, Colorado: Fulcrum 176 pp.
     Muir, J. 1913. The Story of My Boyhood and Youth. Boston: Houghton Mifflin 293 pp.
     Muir, J. 1917. The Cruise of the Corwin. Boston: Houghton Mifflin 278 pp.
5

     Turner, F. 1985. John Muir: Rediscovering America. Cambridge, Massachusetts: Perseus 417 pp.

Christopher K. Starr
Dep't of Life Sciences
University of the West Indies
ckstarr@gmail.com

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Book Review; Travels in Alaska

  • 1. 1 TAKE A WALK ON THE WILD SIDE Review of: John Muir 1915. Travels in Alaska. Boston: Houghton Mifflin 326 pp. [Eighteenth in a series on "naturalist-in" books.] _________________________________________________________________ John Muir (1838-1914) was born in Scotland and immigrated with his family to the USA when he was 11. His early life was marked by hard labour on the family farm in Wisconsin, under his hard-driving calvinist father. He was largely self-taught and showed a genius for inventing and building mechanical devices, including several rather elaborate wooden clocks. Much has been written about Muir and his life, including at least one full-length biography (Turner 1985). A large part (possibly most) of Muir's published writings are available at http://www.yosemite.ca.us/john_muir_writings/ . Muir was a man of robust health and great physical strength, which served him well in his wilderness wanderings. He did a great deal of mountain climbing in western North America, but for him this was not a sport. Rather, he did it to gain a first-hand acquaintance with the land forms and vegetation of areas that had not yet been mapped. And to surround himself with wildness. The opening sentence of his autobiographical The Story of my Boyhood and Youth goes to the heart of what he was all about: "When I was a boy in Scotland, I was fond of everything that was wild, and all my life I've been growing fonder and fonder of wild places and wild creatures." The term "creatures" should be understood broadly to include plants, in which Muir was at least as much interested as he was in animals. His writings show a keen sense of the
  • 2. 2 relationship between plants and habitats. Muir was largely self-taught in scientific subjects, but he came to be respected by the leading natural scientists of his time. He is best known today as a pioneer of the North-American conservation movement, founder of the Sierra Club, and one who helped to create the American National Parks Service. He had a special affinity for California's Sierra Nevada and campaigned for the preservation of some of the most celebrated natural sites in the USA. His main original contribution to science was in the area of how glaciers shape landscapes. Alaska was acquired by the USA from Russia in 1867. Muir first went there in 1879, because "To the lover of pure wilderness Alaska is one of the most wonderful countries in the world." In the trips described in this book, his attention was mainly to the southeastern part of the territory, especially Wrangell Island and the area around the Stickeen River on the nearby mainland. This does not match the popular view of Alaska. It is a cold-temperate region, a cool rain forest without climatic extremes. It is far south of the Arctic Circle, and there is no 24-hour daylight in summer. Even so, the mid-summer sun sets only for a few hours just below the horizon. Another book, The Cruise of the Corwin, tells of a trip to the farther north. Muir had a great deal of contact with native peoples and was even adopted into one tribe. However, he has surprisingly little to say about them. While he was sympathetic and felt generally at home among them, he seemed not especially interested in the human element of the region. On the other hand, his Alaska writings devote much attention to glaciers. Caribbean people can be forgiven a certain
  • 3. 3 unfamiliarity with glaciers, but in some regions they are such a prominent part of the landscape that there is at least one field guide devoted to them (Ferguson 1992). There are several types of glaciers, but we normally associate the term with valley glaciers, the type studied by Muir. You can think of these as high rivers of ice, flowing very slowly down the valley. Ice is constantly breaking off at the lower end, giving rise to icebergs if this is at the sea. Their formation requires quite specific climatic conditions, most particularly high snowfall in winter, followed by a cool winter, so that much of the winter accumulation of snow is not lost before the next winter. Over time the snow is compacted into a mass of ice that flows outward and downward under its own weight. These conditions are of course mainly found in polar and high alpine regions. Although slow, a glacier is a very powerful thing. By its tremendous weight, it carries and pushes large masses of earth and rock as it advances and can be a major force in shaping the landscape through which it moves. Fjords, such as those in Norway and Alaska, are long, narrow coastal valleys with steep sides and rounded bottoms, originally carved out by glaciers. Glaciers are dynamic entities. They constantly change as ice is added in one part and lost in another. Furthermore, they grow and shrink in response to climatic changes. During much of the last ice age, which ended about 11,000 years ago, glaciers covered almost one-third of the land surface of the planet, versus about one-tenth today. We are now between ice ages. Even so, eight minor glaciation cycles have been identified during the past 750,000 years, the most recent from the 17th to the late 19th
  • 4. 4 centuries. In this period, average temperatures were cool enough to permit glaciers to grow significantly. Since Muir's time, in contrast, they have been in overall retreat worldwide. Photos of major valley glaciers taken at intervals of decades commonly show marked changes in size. Even so, at present about three-quarters of the world's fresh water is bound up in glaciers. Global warming causes a rise in the sea level by releasing more of this water into the oceans. Muir seems to have spent much of his time in Alaska in a state of exaltation. At one point he remarks that "When sunshine, sifting through the midst of the multitude of icebergs that fill the fiord and through the jets of radiant spray ever rising from the tremendous dashing and splashing of the falling and upspringing bergs, the effect is indescribably glorious." And elsewhere: "I reached the top of the highest, when one of the greatest and most impressively sublime of all the mountain views I have ever enjoyed came full in sight -- more than three hundred miles of closely packed peaks of the great Coast Range, sculptured in the boldest manner imaginable, their naked tops and dividing ridges dark in colour, their sides and the canyons, gorges and valleys between them loaded with glaciers and snow. From this standpoint I counted upwards of two hundred glaciers." As long as there are truly wild places on Earth, the spirit of John Muir will live among us. References Ferguson, S.A. 1992. Glaciers of North America: A Field Guide. Golden, Colorado: Fulcrum 176 pp. Muir, J. 1913. The Story of My Boyhood and Youth. Boston: Houghton Mifflin 293 pp. Muir, J. 1917. The Cruise of the Corwin. Boston: Houghton Mifflin 278 pp.
  • 5. 5 Turner, F. 1985. John Muir: Rediscovering America. Cambridge, Massachusetts: Perseus 417 pp. Christopher K. Starr Dep't of Life Sciences University of the West Indies ckstarr@gmail.com