scholarly journals The Glacial History of Nantucket and Cape Cod, with an Argument for a Fourth Centre of Glacial Dispersion in North America

1907 ◽  
Vol 39 (3) ◽  
pp. 189
Author(s):  
F. P. G. ◽  
J. Howard Wilson
Keyword(s):  
North America ◽  
Cape Cod ◽  
Glacial History ◽  
History Of

The bryophytes of Nachvak, northern Labrador, with additional records from Saglek

1986 ◽  
Vol 64 (9) ◽  
pp. 2028-2036 ◽  
Author(s):  
Terry A. Hedderson ◽  
Guy R. Brassard
Keyword(s):  
North America ◽  
North American ◽  
Eastern North America ◽  
Glacial History ◽  
The North ◽  
High Incidence ◽  
History Of

One hundred and thirty-four species of mosses and 18 species of liverworts are reported from Nachvak Fiord and 22 mosses are reported from Saglek Fiord. Nineteen of the mosses had not previously been reported from Labrador and 49 are new to northern Labrador. Seven of the liverworts are new to Labrador. Brophyte species new to eastern North America are Anastrophyllum assimile, Hygrophypnum cochlearifolium (possibly) and Lophozia cavifolia. The record of Lophozia cavifolia represents an addition to the hepatic flora of North America (excluding Greenland). The North American distributions of Hydrogrimmia mollis, Marsupella revoluta and Trichostomum arcticum are mapped. The high incidence of disjunct species in the bryoflora of the Torngat Mountains is discussed in relation to the proposed glacial history of the area.

scholarly journals The Omar Story: The Role of Omars in Assessing Glacial History of West-Central North America

2002 ◽  
Vol 54 (3) ◽  
pp. 257-270 ◽  
Author(s):  
Victor K. Prest ◽  
J. Allan Donaldson ◽  
Howard D. Mooers
Keyword(s):  
North America ◽  
Hudson Bay ◽  
Western Canada ◽  
Field Observations ◽  
Glacial History ◽  
Northern Ontario ◽  
West Central ◽  
History Of

Abstract The direction of Wisconsinan glacial dispersion of distinctive Proterozoic erratics derived from the Belcher Group in southeastern Hudson Bay is shown to have been northwestward, westward and southward for hundreds of kilometres across Hudson Bay, Northern Ontario, western Canada, and several adjoining northern States. The most distinctive of these erratics, termed "omars", are composed of massive siliceous wacke characterized by buff-weathering calcareous concretions; these erratics were derived from the Omarolluk Formation of the Belcher Group, exposed in the Belcher Islands of eastern Hudson Bay, and probably underlying much of the southern part of this inland sea. Far less common but equally distinctive are erratics of red oolitic jasper that were derived from the Kipalu Formation of the Belcher Group. In parallel with the now widely accepted field term "omar", we introduce the term "kipalu" for such erratics of oolitic jasper. A map showing the distribution of the distinctive erratics, in relation to indicators of Wisconsinan glacier movement, provides the basis for inferring at least two discrete glaciations that produced several major ice lobes. This paper summarizes the field observations of numerous Canadian and American earth scientists, traces the evolution of thought on provenance of the distinctive erratics, and outlines the criteria for distinguishing "true" omars from erratics derived from other bedrock sources of concretion-bearing wackes.

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