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Betasso Basin

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Journal Article
Published: 01 August 2011
Vadose Zone Journal (2011) 10 (3): 915–927.
.... Thus, the effect of the rejuvenated incision of Boulder Creek appears to extend a maximum of 1000 m up the Betasso drainage basin, but no less than 500 m. The SSR lines on the western slope show slightly deeper weathering than those on the eastern slopes in the lower portion of the catchment...
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Journal Article
Published: 01 August 2011
Vadose Zone Journal (2011) 10 (3): 900–914.
... the foothills to the Continental Divide of the Colorado Front Range show that the rugged topography drives unique biogeochemical processes, low-elevation basins are closer to N-saturation than previously thought, and that a space-for-time substitution is warranted at the snow/rain transition. ALB...
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Series: GSA Field Guide
Published: 01 January 2013
DOI: 10.1130/2013.0033(01)
EISBN: 9780813756332
...Introduction Figure 1. Schematic illustration showing depositional (white) and erosional (gray) episodes in the central and northern Colorado Piedmont during the Cenozoic. Figure is based on preserved sedimentary record in the Denver Basin (Late Cretaceous to early Tertiary) and Colorado...
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Journal Article
Published: 01 August 2011
Vadose Zone Journal (2011) 10 (3): 858–866.
... al., 2002 ; Dethier et al., 2003 ), and climate change likely affected the balance between weathering and regolith transport on slopes adjacent to the glaciated valleys. Annual runoff ranges from about 10 cm near Boulder to 150 cm in portions of the upper Green Lakes basin ( Barry, 1973...
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