Byung Yong Yu
Biographic Data
| ID | 1340516 |
|---|---|
| NAME | Byung Yong Yu |
| GIVEN NAMES | Byung Yong |
| FAMILY NAME | Yu |
| SIGNATURE | YU B Y |
| AFFILIATIONS | Korea Institute of Science and Technology |
| ORCID | 0000-0001-8058-5288 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2017 |
| LATEST PUBLICATION YEAR | 2020 |
| H-INDEX | 0 |
Asymmetric Hillslope Retreat Revealed from Talus Flatirons on Rock Peak, San Tan Mountains, Arizona, United States
Talus flatirons (TFs) are morphostratigraphic markers of prior talus deposition that are now disconnected from the active hillslope. Three generations of TFs (TF1, TF2, TF3) exist flanking a Sonoran Desert inselberg, Rock Peak, in a welded tuff caprocks-controlled landscape bounded by pediments. TFs at Rock Peak enable estimation of slope retreat rates through the application of cosmogenic 10Be, optically stimulated luminescence dating, and catch…
Bouldery slope landforms on Mt. Biseul, Korea, and implications for paleoclimate and slope evolution
Identification of bouldery landforms in mountains and correctly understanding their formative processes play an important role in reconstructing the geomorphic history of a region. We propose that blocks were liberated by frost cracking and wedging of cliff walls during the last glacial period. However, we further suggest and test four hypotheses comprising different scenarios for preconditioning by chemical weathering and subsequent block transp…
No prominent works on this page.
Bouldery slope landforms on Mt. Biseul, Korea, and implications for paleoclimate and slope evolution
Identification of bouldery landforms in mountains and correctly understanding their formative processes play an important role in reconstructing the geomorphic history of a region. We propose that blocks were liberated by frost cracking and wedging of cliff walls during the last glacial period. However, we further suggest and test four hypotheses comprising different scenarios for preconditioning by chemical weathering and subsequent block transp…
Asymmetric Hillslope Retreat Revealed from Talus Flatirons on Rock Peak, San Tan Mountains, Arizona, United States
Talus flatirons (TFs) are morphostratigraphic markers of prior talus deposition that are now disconnected from the active hillslope. Three generations of TFs (TF1, TF2, TF3) exist flanking a Sonoran Desert inselberg, Rock Peak, in a welded tuff caprocks-controlled landscape bounded by pediments. TFs at Rock Peak enable estimation of slope retreat rates through the application of cosmogenic 10Be, optically stimulated luminescence dating, and catch…
Denudation (2 works) · Geochemistry (2 works) · Geology and Paleoclimatology Research (2 works) · Landform (2 works) · Tectonics (2 works) · Alluvium (1 work) · Archaeology (1 work) · Caprock (1 work) · Climate change (1 work) · Colluvium (1 work)