Geomorphology and landforms
From GeoClasses
Contents |
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topography
- map the auditorium topography
- what would be the strike and dip of a bed that was resting on the edges of the risers (at an angle)?
- in real geologic environments, you can't see the entire rock surface - you only get points of information where rocks are exposed (remember field trip).
- if you only had a few random elevation points in this room, what kind of map would you have ended up with? What if all your points were along one riser?
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Carol's topo maps: 1902 and present
- be able to identify major features on topographic maps
- tie back to structures and terrains
- case studies for mass wasting?
- topography before and after - if order new maps that correspond to Carol's old ones
- what caused the event
- stratigraphic columns to find weak layers
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discuss Hooke, 2000 reading
- human influences on topography, erosion and deposition
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Frankel and Pazzaglia, 2006
- go through Frankel and Pazzaglia, 2006 paper
- Taos Range: tectonically active, many landslides
- Sierra Nacimiento: erosionally exhumed, no landslides (once resistant beds were exposed by erosion, river incision is driven by the dropping of base level to the south)
- see google maps here
- east of Sierra Nacimiento site - Valle Caldera near Los Alamos (impact crater)
- figure 9
- what is Rva? figure 6
- ratio of drainage basin volume to drainage basin area
- what is Rva? figure 6
- figure 10
- see google maps here

