The big movement of the fall migration finally began to materialize on
Sunday, August 24. This and the next few days were filled with memorable
experiences. The throngs of Caribou passing at such times around the
head of Windy Bay and across the lowermost portions of Little and Windy
rivers may be accounted for, in part, by the local topography (map 1).
The upper part of Windy Bay, occupied by numerous islands of various
sizes and extending about 5 miles in an east-west direction, opposes
something of a barrier to the Caribou in their southward trek. The
easiest way to overcome this barrier is to by-pass it. So the migrant
herds approaching the north shore of the bay turn westward toward Little
River. At a point half a mile short of this stream a rather minor
proportion of the Caribou actually do essay a passage of Windy Bay. They
cross an island lying very close to the north shore, then steer for a
small rocky islet a quarter of a mile northwest of the mouth of South
Bay. Here they get a brief respite from swimming by walking through the
shallow bordering waters, then continue straight on to the rugged south
shore of Windy Bay. This course is roughly parallel to, and a quarter of
a mile west of, the one pursued northward or northeastward across the
ice in the spring migration. The Caribou were seen to follow this water
route on various days from August 24 to September 8, and again on
October 7. Like the one across the ice, it is probably a regular,
well-established, annual route.
The greater number of the migrants proceed along the north shore of the
bay to Little River and are there confronted with a choice of various
further routes. Some continue for an indefinite distance up the
northeastern bank, passing Lake Charles on their right, though other
animals, coming from the north, may be following this bank in the
opposite direction. Probably most of the Caribou arriving from the
eastward either plunge into Little River at its mouth and swim across
(figs. 9, 10, 12) or pass upstream for a bare quarter of a mile and then
wade across at a rapid (figs. 7, 8).
Public-domain text, read in full here on John Shaqi.
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