... 1999) or an initial erosion rate (Granger et al. ... The location of the bounding curves is d... more ... 1999) or an initial erosion rate (Granger et al. ... The location of the bounding curves is dictated by assumed nuclide production rates. For example, using the currently accepted, high-latitude, sea-level integrated production estimate of 5.2 atoms g –1 y –1 for 10 Be (Bierman et al. ...
A time-dependent, flow-line ice-sheet model is used to explore interactions between last glacial ... more A time-dependent, flow-line ice-sheet model is used to explore interactions between last glacial climate, the Laurentide ice sheet, and the Great Lakes. We seek to understand perturbations in the ice-flow field that caused three neighboring lobes to leave different geomorphic and sedimentary records. Driven by reconstructed air- temperature variations from 65 to 18 ka, the simulated lobe dynamics are consistent
... fluvial dynamics (Potomac River terraces), deciphering the history of arid-region piedmonts (... more ... fluvial dynamics (Potomac River terraces), deciphering the history of arid-region piedmonts (Namibia and South Australia), estimating subaerial bedrock erosion rates (Namibia and Australia), and constraining the magnitude of glacial bedrock erosion (Baffin Island ...
... 1999) or an initial erosion rate (Granger et al. ... The location of the bounding curves is d... more ... 1999) or an initial erosion rate (Granger et al. ... The location of the bounding curves is dictated by assumed nuclide production rates. For example, using the currently accepted, high-latitude, sea-level integrated production estimate of 5.2 atoms g –1 y –1 for 10 Be (Bierman et al. ...
A time-dependent, flow-line ice-sheet model is used to explore interactions between last glacial ... more A time-dependent, flow-line ice-sheet model is used to explore interactions between last glacial climate, the Laurentide ice sheet, and the Great Lakes. We seek to understand perturbations in the ice-flow field that caused three neighboring lobes to leave different geomorphic and sedimentary records. Driven by reconstructed air- temperature variations from 65 to 18 ka, the simulated lobe dynamics are consistent
... fluvial dynamics (Potomac River terraces), deciphering the history of arid-region piedmonts (... more ... fluvial dynamics (Potomac River terraces), deciphering the history of arid-region piedmonts (Namibia and South Australia), estimating subaerial bedrock erosion rates (Namibia and Australia), and constraining the magnitude of glacial bedrock erosion (Baffin Island ...
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