Year |
Citation |
Score |
2017 |
Grant GE, O'Connor JE, Safran E. Excursions in fluvial (dis)continuity Geomorphology. 277: 145-153. DOI: 10.1016/J.Geomorph.2016.08.033 |
0.335 |
|
2015 |
Safran EB, O'Connor JE, Ely LL, House PK, Grant G, Harrity K, Croall K, Jones E. Plugs or flood-makers? The unstable landslide dams of eastern Oregon Geomorphology. 248: 237-251. DOI: 10.1016/J.Geomorph.2015.06.040 |
0.538 |
|
2012 |
Ely LL, Brossy CC, House PK, Safran EB, O'Connor JE, Champion DE, Fenton CR, Bondre NR, Orem CA, Grant GE, Henry CD, Turrin BD. Owyhee River intracanyon lava flows: Does the river give a dam? Bulletin of the Geological Society of America. 124: 1667-1687. DOI: 10.1130/B30574.1 |
0.552 |
|
2011 |
Safran EB, Anderson SW, Mills-Novoa M, House PK, Ely L. Controls on large landslide distribution and implications for the geomorphic evolution of the southern interior Columbia River basin Bulletin of the Geological Society of America. 123: 1851-1862. DOI: 10.1130/B30061.1 |
0.511 |
|
2007 |
Riihimaki CA, Anderson RS, Safran EB. Impact of rock uplift on rates of late Cenozoic Rocky Mountain river incision Journal of Geophysical Research. 112. DOI: 10.1029/2006Jf000557 |
0.639 |
|
2006 |
Safran EB, Blythe A, Dunne T. Spatially variable exhumation rates in orogenic belts: An Andean example Journal of Geology. 114: 665-681. DOI: 10.1086/507613 |
0.7 |
|
2006 |
Riihimaki CA, Anderson RS, Safran EB, Dethier DP, Finkel RC, Bierman PR. Longevity and progressive abandonment of the Rocky Flats surface, Front Range, Colorado Geomorphology. 78: 265-278. DOI: 10.1016/J.Geomorph.2006.01.035 |
0.608 |
|
2005 |
Safran EB, Bierman PR, Aalto R, Dunne T, Whipple KX, Caffee M. Erosion rates driven by channel network incision in the Bolivian Andes Earth Surface Processes and Landforms. 30: 1007-1024. DOI: 10.1002/Esp.1259 |
0.622 |
|
2003 |
Safran EB. Geomorphic interpretation of low‐temperature thermochronologic data: Insights from two‐dimensional thermal modeling Journal of Geophysical Research. 108. DOI: 10.1029/2002Jb001870 |
0.485 |
|
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