. The Canadian field-naturalist. 46 The Canadian Field-Naturalist Vol. 86. Figure 1. Map showing the location of the study areas described in the text. an abrupt termination of the sand and gravel outwash deposit, with barren sand slopes de- scending 50 to 100 feet or more to the surface of coarse boulder and gravel drift possessing the familiar surface features indicating exten- sive former glaciation. A discussion of past climatic relationships of vegetation in the area is provided in the recent discussion by Nichols (1970), a mem- ber of our field party (see Acknowledgements). Pollen diagra
. The Canadian field-naturalist. 46 The Canadian Field-Naturalist Vol. 86. Figure 1. Map showing the location of the study areas described in the text. an abrupt termination of the sand and gravel outwash deposit, with barren sand slopes de- scending 50 to 100 feet or more to the surface of coarse boulder and gravel drift possessing the familiar surface features indicating exten- sive former glaciation. A discussion of past climatic relationships of vegetation in the area is provided in the recent discussion by Nichols (1970), a mem- ber of our field party (see Acknowledgements). Pollen diagrams constructed from the result of pollen analysis of peat monoliths recovered from organic deposits show that the climatic history of the region, as so determined, cor- relates well with the history of other adjacent northern regions, particularly the Ennadai Lake area, as determined by Nichols earlier (see references in Nichols 1970).. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Ottawa Field-Naturalists' Club. Ottawa, Ottawa Field-Naturalists' Club
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