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Volume 4, 1951 - The Arctic Circle - Home

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f the route offered good footing on an elevated gravel<br />

1dge. Exploration of Dawson Bay revealed the presence of<br />

ny lime-loving plants, but perhaps the most interesting<br />

eature is the numerous salt springs around which grow plants<br />

ore normally found along coastal salt marshes. On the return<br />

to the Grand Rapids portage, the lightened canoes were<br />

un down the awe-inspiring rapids, covering in one part a<br />

1stance of two miles in six minutes. <strong>The</strong> party returned<br />

to Winnipeg on the S.S. ~~enoFa, a steamboat originally<br />

lying Lake of the Woods, but rebuilt on Lake Winnipeg, and<br />

now rounding out its ancient life in serving isolated comunities<br />

along the stormy waters of this shallow remuant of<br />

lacial Lake Agassize<br />

Besides the writer, the 1949 field party again inluded<br />

Nick Neufeld and Jim Robinson, together with John<br />

• Campbell of Hamilton, Onta~io. <strong>The</strong> route led down the<br />

elson River from Nc:rway House: across nFainted Stone<br />

ortage" on the height of lal1(}at. the hGadw·~J.te!"s of the<br />

ohimamish, and j.nto the Hayes River system. <strong>The</strong> greater<br />

art of the Hayes lies in th8 Procambrian, and includes a<br />

,hain of lakes bearing the names Robinson, Logan, Max, Windy,<br />

xford, Knee, and S'tJ':é'.mpy" Many portages are necessary in the<br />

ntervening reaches. About hO miles belmv SW8lnPy Lake, or<br />

bout 100 miles above York F~ctory, the river enters the<br />

laeozoic formations of the Hudson Bay Lowlands, and winds<br />

ith great regularity between clay banks )0 to 100 feet<br />

19h, the only obstructions to canoe travel being the<br />

hallowness of the water and the occurrence of gravel bars<br />

t each bend. <strong>The</strong> flora of this section includes many limeoving<br />

species absent from the Precambrian formations to the<br />

est. This is particularly so along the gravel beaches and<br />

ars, where, in the absence of competing forest species,<br />

sses of tansy, arnica, hedysarQffi,arctie vetch, painted-cup,<br />

iver-beauty, and other northern species produce a breathaking<br />

blaze of colour. <strong>The</strong> arctic influence is evident<br />

ound York Factory, where such northern cireQ~polar species<br />

.s a grass (Dupomia Fisheri forma p.§~.lQ..santha), a willow<br />

Salix reticulataJ, and arctic daisy \ ~rysanthemum arcticum)<br />

e found.<br />

Following a week of collecting around York Factory,<br />

he party rounded the shallow and treachercus tidal waters .<br />

ff Marsh Point and entered the estuary of the Nelson. <strong>The</strong><br />

ift water and many rapids of the eighty-mile stretch to<br />

imestone Rapids, at which point contact was made with the<br />

udson Bay Railway, made it necessRry to line the heavily<br />

oaded canoes for conside:"able dis~D.J::.:;9S, psrticularly around<br />

e numerous limestor-e headlands. ~he r8main~ng part of the<br />

eason was spent in the area of Wekasko and Tramping Lakes,

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