A 1000-year record of forest fire, drought and lake-level change in southeastern British Columbia, Canada

The Holocene ◽  
2003 ◽  
Vol 13 (5) ◽  
pp. 751-761 ◽  
Author(s):  
Douglas J. Hallett ◽  
Rolf W. Mathewes ◽  
Robert C. Walker
Keyword(s):  
British Columbia ◽  
Forest Fire ◽  
Lake Level ◽  
Lake Level Change ◽  
Level Change

scholarly journals Late Quaternary tectonic activity and lake level change in the Rukwa Rift Basin

1998 ◽  
Vol 26 (3) ◽  
pp. 397-421 ◽  
Author(s):  
D. Delvaux ◽  
F. Kervyn ◽  
E. Vittori ◽  
R.S.A. Kajara ◽  
E. Kilembe
Keyword(s):  
Lake Level ◽  
Late Quaternary ◽  
Tectonic Activity ◽  
Rift Basin ◽  
Lake Level Change ◽  
Level Change

Lake level change, climate, and the impact of natural events: the role of seismic and volcanic events in the formation of the Lake Patzcuaro Basin, Michoacan, Mexico

2005 ◽  
Vol 135 (1) ◽  
pp. 35-46 ◽  
Author(s):  
I. Israde-Alcántara ◽  
V.H. Garduño-Monroy ◽  
C.T. Fisher ◽  
H.P. Pollard ◽  
M.A. Rodríguez-Pascua
Keyword(s):  
Lake Level ◽  
Lake Level Change ◽  
Level Change ◽  
Volcanic Events ◽  
Lake Patzcuaro Basin ◽  
Change Climate ◽  
The Impact

scholarly journals Expansion of an ancient lake in the Kathmandu basin of Nepal during the Late Pleistocene evidenced by lacustrine sediment underlying piedmont slope

1970 ◽  
Vol 4 (6) ◽  
pp. 41-48
Author(s):  
Kiyoshi Saijo ◽  
Kazuo Kimura
Keyword(s):  
Late Pleistocene ◽  
Lake Level ◽  
Lacustrine Sediments ◽  
Ancient Lake ◽  
Nepal Himalaya ◽  
Lake Level Change ◽  
Level Change ◽  
Muddy Sediments ◽  
Surface Geology ◽  
Bagmati River

We investigated the geomorphology and surface geology of the piedmont slope on the margins of the Kathmandu basin in the Nepal Himalaya in order to establish Late Pleistocene geography and especially the extent of the ancient lake in the basin. The piedmont slope consists of detrital deposits of colluvial or fluvial origin, underlain and interfingered by organic muddy sediments with radiocarbon ages of about 30,000 yr BP. Detritus from the surrounding hillslopes and lacustrine sediments were alternately deposited as the lake level rose at about that time. The ancient lake in the Kathmandu basin thus reached a level of between 1400 and 1440 m at around 30,000 yr BP, when it covered almost the entire basin. Because the cols on the surrounding divide are higher than this estimated lake level, and because reddish soils and weathered bedrock are observed on these cols, we conclude that overflow from an outlet other than the Bagmati River probably did not occur. Drainage of the ancient lake by the Bagmati River began just after 30,000 yr BP. Key words: Nepal, Kathmandu basin, piedmont slope, lacustrine, lake level change, Late Pleistocene Himalayan Journal of Sciences Vol.4(6) 2007 p.41-48

scholarly journals Glacier and lake level change from TOPEX-series and Cryosat-2 altimeters in Tanggula: Comparison with satellite imagery

2021 ◽  
Vol 32 (1) ◽  
pp. 1-20
Author(s):  
Cheinway Hwang ◽  
Shiang-Hung Wei ◽  
Yung-Sheng Cheng ◽  
Adili Abulaitijiang ◽  
Ole Baltazar Andersen ◽  
...  
Keyword(s):  
Satellite Imagery ◽  
Lake Level ◽  
Lake Level Change ◽  
Level Change

Sedimentary noise modeling of lake-level change in the late Triassic Newark Basin of North America

2021 ◽  
pp. 103706
Author(s):  
Meng Wang ◽  
Mingsong Li ◽  
David B. Kemp ◽  
Slah Boulila ◽  
James G. Ogg
Keyword(s):  
North America ◽  
Lake Level ◽  
Late Triassic ◽  
Lake Level Change ◽  
Noise Modeling ◽  
Level Change ◽  
Newark Basin

Geophysical evidence for Holocene lake-level change in southern California (Dry Lake)

Boreas ◽  
2010 ◽  
Vol 39 (1) ◽  
pp. 131-144 ◽  
Author(s):  
BROXTON W. BIRD ◽  
MATTHEW E. KIRBY ◽  
IAN M. HOWAT ◽  
SLAWEK TULACZYK
Keyword(s):  
Lake Level ◽  
Southern California ◽  
Lake Level Change ◽  
Level Change ◽  
Dry Lake
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