Abstract
Morphometric and other relative-age data were collected on early- to late-Pleistocene end moraines located in the Kigluaik Mountains of Seward Peninsula, Alaska. Discriminant analysis indicates that average slope, calculated from the slope-frequency distribution, is the best single distinguishing criterion, and that even a few simple field measurements of morphometry provide a viable basis for subdividing and correlating moraines. Morphometric and other relative-age data constrain the timing of glaciations in the Kigluaik Mountains, and suggest that successively older advances are separated by intervals of increasing duration. -from Authors
| Original language | English (US) |
|---|---|
| Title of host publication | Arctic & Alpine Research |
| Pages | 273-284 |
| Number of pages | 12 |
| Volume | 20 |
| Edition | 3 |
| State | Published - 1988 |
| Externally published | Yes |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Cite this
Morphometric analysis of Pleistocene glacial deposits in the Kigluaik Mountains, northwestern Alaska, USA. / Kaufman, Darrell S; Calkin, P. E.
Arctic & Alpine Research. Vol. 20 3. ed. 1988. p. 273-284.Research output: Chapter in Book/Report/Conference proceeding › Chapter
}
TY - CHAP
T1 - Morphometric analysis of Pleistocene glacial deposits in the Kigluaik Mountains, northwestern Alaska, USA
AU - Kaufman, Darrell S
AU - Calkin, P. E.
PY - 1988
Y1 - 1988
N2 - Morphometric and other relative-age data were collected on early- to late-Pleistocene end moraines located in the Kigluaik Mountains of Seward Peninsula, Alaska. Discriminant analysis indicates that average slope, calculated from the slope-frequency distribution, is the best single distinguishing criterion, and that even a few simple field measurements of morphometry provide a viable basis for subdividing and correlating moraines. Morphometric and other relative-age data constrain the timing of glaciations in the Kigluaik Mountains, and suggest that successively older advances are separated by intervals of increasing duration. -from Authors
AB - Morphometric and other relative-age data were collected on early- to late-Pleistocene end moraines located in the Kigluaik Mountains of Seward Peninsula, Alaska. Discriminant analysis indicates that average slope, calculated from the slope-frequency distribution, is the best single distinguishing criterion, and that even a few simple field measurements of morphometry provide a viable basis for subdividing and correlating moraines. Morphometric and other relative-age data constrain the timing of glaciations in the Kigluaik Mountains, and suggest that successively older advances are separated by intervals of increasing duration. -from Authors
UR - http://www.scopus.com/inward/record.url?scp=0024258224&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0024258224&partnerID=8YFLogxK
M3 - Chapter
AN - SCOPUS:0024258224
VL - 20
SP - 273
EP - 284
BT - Arctic & Alpine Research
ER -