FINAL REVIEW SHEET (for old material) - material
since last exam will also be about half of the final! – check
out practice questions/diagrams on website!
STUFF IN RED IS ESPECIALLY IMPORTANT; Review old exam questions related to these topics; Also, check out old “lecture diagrams” for topics not discussed in the book…
Chapters 11 and 12 – Earth Interior/Plate Tectonics/Mountain
Building/Earthquakes/Volcanos
- thus convergent, divergent, and transform (i.e. San Andreas) plate boundaries
·
Orogenesis
· Rocky Mountains à Laramide Orogeny
· Fault Block Mountains - Sierra Nevada mtns (batholith/pluton); Tetons; Basin and Range
·
Fold and
o Canadian
o
· Folding/Faulting
o Brittle vs Ductile deformation
o Types of folds and faults (normal, reverse, thrust, strike-slip); Horst and Graben – Basin and Range; San Andreas Fault – “Strike-Slip”
·
Earthquakes – where are
they?
o Focus, Epicenter
o Moment Magnitude Scale
o Geomorphic Effects: Landslides, Liquefaction, Tsunamis
·
Volcanoes
·
Type of magma in
relation to plate tectonics
·
Composite Cone/Stratovolcano – Explosive
· Cinder Cone/Caldera/Pyroclastic Flow/Lahar
· Volcanic Neck/Dike/Batholith/Pluton/Laccolith
·
Hot Spots –
·
Chapters 13 and 18 – Weathering, Soils, Mass Wasting
· Chemical
§ Spheroidal Weathering
§ Hydrolysis, oxidation, carbonation (Karst topography)
· Soils
o Classes of Mass movements
Chapters 9 and 14 – Ground Water/Surface Water/Flooding/Fluvial
Processes/Fluvial Landforms
· Groundwater
o Infiltration, percolation, water table
o Permeability and porosity (hydraulic conductivity)
o Aquiclude/Springs
o Aquifer – confined vs. unconfined
§ Unconfined – wells, drawdown/cone of depression
· Darcy’s Law – rate of groundwater flow: q=h/l x K
· High Plains Aquifer/Denver Basin
§ Confined – Artesian Well, potentiometric surface; Black Hills
o Groundwater Problems: subsidence, drawdown, saltwater, pollution
§ Drainage Networks
§ Hydrographs
§ Flooding:
§ Dams: Ecological Effects of decreased flooding downstream from dams
§ Fluvial Forms and Processes
§ River Discharge: width x depth x velocity = Q
§ Longitudinal Profile – channel gradient decreases to base
level or local base level
§ Shear Stress: Determines amount of sediment a river can carry
§ Sediment Load: dissolved, suspended, bed load (how do these
relate to channel form)
§ Channel Form
·
Meandering River
Landforms: oxbow, point bar, etc…
· Mountain streams types; relation to channel slope; How is grain size related to channel slope and shear stress downstream along a longitudinal profile
· Graded Stream
· Nickpoints
· Sediment Deposition
o Floodplains
o Terraces – factors related to how they form
o
Deltas
– ultimate sediment destination; Miss. R. Delta