scholarly article | Q13442814 |
P819 | ADS bibcode | 2020JGRF..12505260S |
P356 | DOI | 10.1029/2019JF005260 |
P2093 | author name string | D. J. Ward | |
C. E. Sheehan | |||
P2860 | cites work | Evidence for nonlinear, diffusive sediment transport on hillslopes and implications for landscape morphology | Q29542478 |
Dynamic reorganization of river basins | Q47664778 | ||
Formation of the Grand Canyon 5 to 6 million years ago through integration of older palaeocanyons | Q56082871 | ||
Creative computing with Landlab: an open-source toolkit for building, coupling, and exploring two-dimensional numerical models of Earth-surface dynamics | Q57455485 | ||
An uplift history of the Colorado Plateau and its surroundings from inverse modeling of longitudinal river profiles | Q57867348 | ||
Steady state, erosional continuity, and the topography of landscapes developed in layered rocks | Q57893988 | ||
Block-controlled hillslope form and persistence of topography in rocky landscapes | Q57978335 | ||
Chronology and paleoenvironmental interpretation of talus flatiron sequences in a sub-humid mountainous area: Tremp Depression, Spanish Pyrenees | Q58027202 | ||
Colorado River chronostratigraphy at Lee's Ferry, Arizona, and the Colorado Plateau bull's-eye of incision | Q58078149 | ||
THE INFLUENCE OF PLEISTOCENE CLIMATES UPON THE MORPHOLOGY OF CUESTA SCARPS ON THE COLORADO PLATEAU1 | Q58138036 | ||
Palaeoclimatic considerations of talus flatirons and aeolian deposits in Northern Fuerteventura volcanic island (Canary Islands, Spain) | Q58594120 | ||
Are talus flatiron sequences in Spain climate-controlled landforms? | Q58894870 | ||
Considerations on the chronological and causal relationships between talus flatirons and palaeoclimatic changes in central and northeastern Spain | Q58894875 | ||
Complexities of landscape evolution during incision through layered stratigraphy with contrasts in rock strength | Q59786840 | ||
Rapid incision of the Colorado River in Glen Canyon - insights from channel profiles, local incision rates, and modeling of lithologic controls | Q64352999 | ||
Cosmogenic 3He exposure ages of Pleistocene debris flows and desert pavements in Capitol Reef National Park, Utah | Q64862889 | ||
Late Pleistocene talus flatiron formation below the Coal Cliffs cuesta, Utah, USA | Q70676794 | ||
Dip, layer spacing, and incision rate controls on the formation of strike valleys, cuestas, and cliffbands in heterogeneous stratigraphy | Q73303382 | ||
6 Ma age of carving Westernmost Grand Canyon: Reconciling geologic data with combined AFT, (U–Th)/He, and 4He/3He thermochronologic data | Q74779168 | ||
Cosmogenic dating of fluvial terraces, Fremont River, Utah | Q97323420 | ||
New incision rates along the Colorado River system based on cosmogenic burial dating of terraces: Implications for regional controls on Quaternary incision | Q97431102 | ||
Relict slope rings and talus flatirons in the Colorado Piedmont: Origin, chronology and paleoenvironmental implications | Q105620192 | ||
P433 | issue | 3 | |
P577 | publication date | 2020-03-01 | |
P1433 | published in | Journal of Geophysical Research. Earth Surface | Q27726645 |
P1476 | title | Migrating Transverse Escarpments in Strike Valleys on the Colorado Plateau | |
P478 | volume | 125 |
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