Norman P Lasca
Biographic Data
| ID | 5592124 |
|---|---|
| NAME | Norman P Lasca |
| GIVEN NAMES | Norman P |
| FAMILY NAME | Lasca |
| SIGNATURE | LASCA N P |
| AFFILIATIONS | University of Wisconsin–Milwaukee |
| VERIFIED | No |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1966 |
| LATEST PUBLICATION YEAR | 1999 |
| H-INDEX | 0 |
Oriented lake-and-ridge assemblages of the Arctic coastal plains
Oriented assemblages of parallel ridges and elongated lakes are widespread on the coastal lowlands of northeast Eurasia and Arctic North America, in particular, in Alaska, Arctic Canada, and northeast Siberia. So far, only the oriented lakes have been of much scientific interest. They are believed to be formed by thermokarst in perennially frozen ice-rich sediments, while their orientation is accounted for either by impact of modern winds blowing…
Animals at the North Pole
An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content
Archaeological geology of North America
Postglacial Delevelling in Skeldal, Northeast Greenland
Skeldal is a northeast-trending valley in the Mesters Vig district, on the southwest shore of Kong Oscars Fjord, about 70 km from the fiord's entrance, in the northeast corner of Scoresby Land. Thirteen radiocarbon dates of shell material which were used to establish a rate of emergence in Skeldal, indicate that the valley was partially open to the sea by ca 8500 BP. Early emergence (8000-7000 BP) was approx 3 m/century. Emergence is related almo…
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Postglacial Delevelling in Skeldal, Northeast Greenland
Skeldal is a northeast-trending valley in the Mesters Vig district, on the southwest shore of Kong Oscars Fjord, about 70 km from the fiord's entrance, in the northeast corner of Scoresby Land. Thirteen radiocarbon dates of shell material which were used to establish a rate of emergence in Skeldal, indicate that the valley was partially open to the sea by ca 8500 BP. Early emergence (8000-7000 BP) was approx 3 m/century. Emergence is related almo…
Archaeological geology of North America
Animals at the North Pole
An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content
Oriented lake-and-ridge assemblages of the Arctic coastal plains
Oriented assemblages of parallel ridges and elongated lakes are widespread on the coastal lowlands of northeast Eurasia and Arctic North America, in particular, in Alaska, Arctic Canada, and northeast Siberia. So far, only the oriented lakes have been of much scientific interest. They are believed to be formed by thermokarst in perennially frozen ice-rich sediments, while their orientation is accounted for either by impact of modern winds blowing…
Geography (3 works) · Geology (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (2 works) · Glacial period (2 works) · Oceanography (2 works) · Oceanography (2 works) · Paleontology (2 works) · Paleontology (2 works) · Physical geography (2 works)