Did rock avalanche deposits modulate the late Holocene advance of Tiedemann Glacier, southern Coast Mountains, British Columbia, Canada?

Author:

Menounos Brian,Clague John J.,Clarke Garry K.C.,Marcott Shaun A.,Osborn Gerald,Clark Peter U.,Tennant Christina,Novak Anthony M.

Funder

Natural Sciences and Engineering Research Council of Canada

Canadian Foundation for Climate and Atmospheric Sciences (Western Canadian Cryospheric Network)

Geological Society of America

National Science Foundation (NSF)

Oregon State University

NSF

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference67 articles.

1. Late Holocene vegetation and climate change at Moraine Bog, Tiedemann Glacier, southern Coast Mountains, British Columbia;Arsenault;Can. J. Earth Sci.,2007

2. Earthquake recurrence inferred from paleoseismology;Atwater;Dev. Quat. Sci.,2004

3. 10Be ages of late Pleistocene deglaciation and Neoglaciation in the north–central Brooks Range, Arctic Alaska;Badding;J. Quat. Sci.,2012

4. Regional beryllium-10 production rate calibration for late-glacial northeastern North America;Balco;Quat. Geochronol.,2009

5. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements;Balco;Quat. Geochronol.,2008

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