Supplemental Material: Early Pleistocene climate-induced erosion of the Alaska Range formed the Nenana Gravel
- Rachel Sortor (11251281)
- et al. (281964)
DOIAbstract
Expanded methods, discussion of outliers, sample data and supplemental figures.<br
Expanded methods, discussion of outliers, sample data and supplemental figures.<br
Human colonization and subsequent occupation of eastern Beringia, beginning c. 14,500 years ago, is ...
The CRREL permafrost tunnel offers a unique opportunity to sample ice wedges in a climate-controlled...
Nonglaciated lowlands in central and southwestern Alaska contain extensive deposits of upper-Quatern...
Thesis (M.S.) University of Alaska Fairbanks, 2000Facies architecture analysis, lithostratigraphy, a...
The overall goal of this project is to use variations in sediment source through time as a proxy fo...
1979 and 1984 recovered stone tools within and below paleosol stringers dated between 8160 ± 260 14C...
Item S1: Physiographic aspects of the Wrangell Arc that make bedrock sampling challenging, including...
Numerous exposures of Pleistocene sediments occur in the Noatak basin, which extends for 130 km alon...
International audienceErosion related to glacial activity produces enormous amounts of sediment. How...
From introduction: The history of glaciation in Alaska offers a fascinating field for study. Because...
Glacial landforms and outwash terraces in the Nenana River valley, Reindeer Hills and Monahan Flat i...
The research presented here seeks to constrain the multiple episodes of uplift and denudation contri...
Southwestern Alaska is a critically understudied region of Beringia, highlighted by the lack of pale...
Analytical methods, regional geological summary, zircon age compilation, and statistical testing of ...
Graduation date: 2005Sediment storage in and release from the Granite Creek catchment over Holocene ...
Human colonization and subsequent occupation of eastern Beringia, beginning c. 14,500 years ago, is ...
The CRREL permafrost tunnel offers a unique opportunity to sample ice wedges in a climate-controlled...
Nonglaciated lowlands in central and southwestern Alaska contain extensive deposits of upper-Quatern...
Thesis (M.S.) University of Alaska Fairbanks, 2000Facies architecture analysis, lithostratigraphy, a...
The overall goal of this project is to use variations in sediment source through time as a proxy fo...
1979 and 1984 recovered stone tools within and below paleosol stringers dated between 8160 ± 260 14C...
Item S1: Physiographic aspects of the Wrangell Arc that make bedrock sampling challenging, including...
Numerous exposures of Pleistocene sediments occur in the Noatak basin, which extends for 130 km alon...
International audienceErosion related to glacial activity produces enormous amounts of sediment. How...
From introduction: The history of glaciation in Alaska offers a fascinating field for study. Because...
Glacial landforms and outwash terraces in the Nenana River valley, Reindeer Hills and Monahan Flat i...
The research presented here seeks to constrain the multiple episodes of uplift and denudation contri...
Southwestern Alaska is a critically understudied region of Beringia, highlighted by the lack of pale...
Analytical methods, regional geological summary, zircon age compilation, and statistical testing of ...
Graduation date: 2005Sediment storage in and release from the Granite Creek catchment over Holocene ...
Human colonization and subsequent occupation of eastern Beringia, beginning c. 14,500 years ago, is ...
The CRREL permafrost tunnel offers a unique opportunity to sample ice wedges in a climate-controlled...
Nonglaciated lowlands in central and southwestern Alaska contain extensive deposits of upper-Quatern...
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