Results 121 to 130 of about 215 (158)
Some of the next articles are maybe not open access.

Related searches:

Neoglacial Lake Alsek

Canadian Journal of Earth Sciences, 1982
Lowell Glacier, a large valley glacier in the St. Elias Mountains of southwestern Yukon Territory, advanced across Alsek Valley and blocked south-flowing Alsek River many times during the Neoglacial interval. The resulting lake, termed Neoglacial Lake Alsek, extended east of the front of the St.
John J. Clague, V. N. Rampton
openaire   +2 more sources

Neoglaciation in western Norway—preliminary results

Norsk Geografisk Tidsskrift - Norwegian Journal of Geography, 1979
An attempt to reconstruct the neoglacial pattern in western Norway is done by measurements of the lichen Rh. geogr. agg. on moraine ridges in the marginal zones at 9 selected glaciers (Fig. 1). Differences in the fluctuations of the glaciers are briefly discussed.
Nils Hole, Johan Ludvig Sollid
openaire   +1 more source

Neoglaciation in the southern Coast Mountains of British Columbia: chronology prior to the late Neoglacial maximum

Canadian Journal of Earth Sciences, 1986
Moraine stratigraphy and morphology, radiocarbon dates from Klinaklini, Franklin, Tiedemann, Gilbert, and Bridge glaciers, and related information from elsewhere in the Coast Mountains are used to construct a chronology for glacier fluctuations.
J. M. Ryder, B. Thomson
openaire   +1 more source

Neoglaciation in South Norway using lichenometric methods

Norsk Geografisk Tidsskrift - Norwegian Journal of Geography, 1986
The neoglacial history of South Norway is illuminated through a lichenometric study of 14 ice-marginal zones of glaciers situated along a right angled line running north-south and west-east to cover a vast area. Maps of the marginal zones two lichen growth curves, the moraine dates and a frequency diagram are presented on a plate, PI. 1.
Lars Erikstad, Johan Ludvig Sollid
openaire   +1 more source

Neoglaciation in the Spanish Pyrenees: a multiproxy challenge

Mediterranean Geoscience Reviews, 2020
Following the Holocene Thermal Maximum, dated between 11 and 6 ka, the Neoglacial period was one of the progressive, fluctuating cooling that peaked during the Little Ice Age (LIA). The almost total absence of glacial tills prior to the LIA in the Pyrenees forces recourse to a high variety of proxies, including lacustrine sediments, palynological ...
José M. García-Ruiz   +3 more
openaire   +1 more source

Neoglacial Glacier Fluctuations in the Canadian Rockies

Quaternary Research, 1993
AbstractThe Little Ice Age was the most extensive Neoglacial glacier advance in the Canadian Rockies. Evidence of earlier, less-extensive Neoglacial glacier advances is based on wood recovered from several glacier forefields. Wood flushed out of Athabasca Glacier (7550-8230 yr B.P., three dates) and Dome Glacier (6120-6380 yr B.P., two dates) indicates
Brian H. Luckman   +2 more
openaire   +1 more source

Neoglacial chronology, northeastern Saint Elias Mountains, Canada

American Journal of Science, 1966
Drift morphology, stratigraphy, and C-14 dates suggest chronology for Donjek and Kaskawulsh Glaciers. About 12,500 B.P. Kluane glaciers receded from near Kluane Lake and about 9780 B.P. withdrew behind present Kaskawulsh moraines. During Slims nonglacial interval, glaciers maintained retracted positions; Kaskawulsh terminus was located at least 13.7 ...
G. H. Denton, M. Stuiver
openaire   +1 more source

Stratigraphy of a Neoglacial end moraine in Norway

Boreas, 1973
There exposures in an outer end moraine ridge at Autre Okstindbredal, north Norway, are described and interpreted. The presence of perennially frozen ground is attributed to the present or very recent climate of the area and suggest the occurence of true sporadic permafrost.
MICHAEL J. ALEXANDER, PETER WORSLEY
openaire   +1 more source

Evidence of Neoglacial Solifluction at Okstindan, North Norway

ARCTIC, 1974
A section excavated through two adjacent turf-banked solifluction lobes has revealed buried soils beneath each solifluction sheet. Five radiocarbon dates are reported from the buried soils and these reveal evidence of soil movement which probably extends over nearly 3,000 years until the present.
Peter Worsley, Charles Harris
openaire   +1 more source

Home - About - Disclaimer - Privacy