| Title | Quaternary geology and glacial history of Bylot Island, Northwest Territories |
| Download | Downloads |
| Licence | Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences. |
| Author | Klassen, R A |
| Source | Geological Survey of Canada, Memoir 429, 1993, 93 pages, https://doi.org/10.4095/183984 (Open Access) |
| Year | 1993 |
| Document | serial |
| Lang. | English |
| Maps | Publication contains 1 map |
| Map Info. | surficial geology, lithology, 1:250,000 |
| Media | paper; on-line; digital |
| Related | This publication contains Klassen, R A; (1993). Surficial
geology, Bylot Island and adjacent areas, District of Franklin, Northwest Territories, Geological Survey of Canada, "A" Series Map no. 1686A |
| File format | pdf |
| Province | Nunavut |
| NTS | 38C; 38B; 38A/03; 38A/04; 38A/05; 38A/06; 38A/11; 38A/12; 38A/13; 38A/14; 38C/01; 38C/02; 38C/03; 38C/04; 38C/05; 38C/06; 38C/07; 38C/08; 38C/09; 38C/10; 38C/11; 38C/12; 38D/03; 38D/04; 38D/05; 38D/12;
48A/01; 48A/08; 48A/09; 48A/16; 48D/01; 48D/08; 48D/09 |
| Area | Bylot Island; Baffin Island |
| Lat/Long WENS | -81.0000 -74.0000 73.7500 72.0000 |
| Subjects | geochronology; surficial geology/geomorphology; paleontology; radiocarbon dates; radiometric dates; colluvial deposits; eolian deposits; alluvial deposits; marine deposits; glaciofluvial deposits;
glaciolacustrine deposits; drift deposits; glaciation; moraines; eskers; glacial deposits; depositional environment; glacial history; provenance; glacial stages; Holocene; glaciers; ice sheets; sea level fluctuations; paleobotany; invertebrates;
biostratigraphy; macrofossils; fossil plants; fossils; Arthropoda; amino acid ratios; Quaternary |
| Illustrations | sketch maps; photographs; stratigraphic columns; aerial photographs; analyses |
| Released | 1993 05 01; 2014 02 07 |
| Abstract | The Quaternary geology of Bylot Island records glaciation by regional ice sheets and by local mountain glaciers, and marine and glaciomarine sedimentation around its margins. The geological evidence for
the last major foreign glaciation, Eclipse glaciation, is widespread in surficial deposits and landforms and is used as a basis for recognition of other glacial events and for establishing their relative ages. Four distinct foreign glaciations are
recognized. The oldest and most extensive, named Baffin glaciation, occurred prior to a period of interglacial weathering, named Salmon River interglaciation, and ice could have moved northward across the topographic divide of Bylot Island. During
the later Eclipse glaciation, ice was less extensive, although it fully occupied the channels around the island and attained elevations of 270 to 370 m a.s.l. from 10 to 20 km inland on the south coast, and 500 to 600 m a.s.l. against the northern
coastal mountains. Eclipse glaciation occurred prior to 43 000 radiocarbon years ago and is older than marine shells having amino acid ratios (D-alloisoleucine to L-isoleucine) of 0.20 to 0.25. Evidence of the younger Button glaciation is restricted
to coastal areas of Bylot Island below 140 m a.s.l., and foreign ice was restricted to the marine channels and was likely floating. Button drift is bounded stratigraphically by shells having amino acid ratios of about 0.15 and 0.10. Cape Hatt
glaciation is of Late Wisconsinan or early Holocene age during which time ice extended across Baffin Island to the northern mouth of Milne Inlet. Three periods of native glaciation are known. The oldest, named Bylot glaciation, was most extensive and
covered most of the island prior to Baffin glaciation. Late during Eclipse glaciation, native glaciers that had been dammed on the island by foreign ice underwent major expansion as part of Aktineq glacial phase as they re-established normal outward
directions of flow. Modern glaciers appear to be either stationary at, or retreating from, Neoglacial maximum positions attained within the last 100 years that represent their greatest extent since Eclipse glaciation. Five periods of change in
relative sea level are recognized, the oldest of which predates Salmon River interglaciation and is represented in sections by marine sediments containing in situ shells with amino acid ratios of 0.55 to 0.60. Younger marine sediments of pre-Eclipse
age occur in two stratigraphic sections and contain shells having amino acid ratios of about 0.4 to 0.35. Surficial marine sediments of pre-Holocene age are related to periods of higher relative sea level subsequent to Eclipse glaciation and to
Button glaciation. They contain shells having amino acid ratios of about 0.2 and 0.1, respectively. Eclipse marine sediments may extend to 90 m a.s.l. near Canada Point. On northern Bylot Island, Button marine sediments extend to 35 m a.s.l. Holocene
emergence is 100 mat the southern end of Milne Inlet, 80 mat Cape Hatt, 50 to 60 m near Pond Inlet townsite, and 35 to 45 m on southern Bylot Island. No raised Holocene marine sediments are known on northern Bylot Island and there the modern coast
appears to be submerging. |
| GEOSCAN ID | 183984 |
|
|