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Geology 140-Honors
Test 1
| Question | Answer |
|---|---|
| Geology | science concerned with study of earth, composition, process, and history |
| Water (resource) | 70% of earth's surface. we drink from groundwater (rivers/streams) cone of depression-from wells ground water is stored in aquifers |
| Strike-Slip Fault | two plates slide past one another |
| Reverse fault | The hanging wall moves up |
| Normal fault | Hanging wall moves down |
| Breaks in Rock | Creates faults. 1. Normal 2. Reverse 3. Strike-slip |
| Bending in Rocks | Creates folds 1. anticline (rocks arch) 2. syncline (rock sinks) |
| Metamorphic Rocks | For by recrystallization of existing rocks under heat and pressure. |
| Sedimentary Rocks | Form by lithification of sediment (sand, silt, clay, shells) |
| Lithification | 1. cement together 2. compact together |
| Igneous Rock | For by solidification of molten rock (magma and lava) |
| Type of Rocks | Igneous Sedimentary Metapmorphic |
| Hot spots | Convective upwelling of hot material from deep within the mantle (yellowstone) fixed position in mantle |
| Transform Plate Boundary | Result from shear stress Plates slide past each other Associated with mid-ocean ridges (San Andres Fault) |
| Convergent Plate boundaries | compressional subduction creates volcanoes 1)ocean-ocean:older cooler crust subducts (volcanoes) 2)Ocean-continent:ocean crust subducts (volcanoes) 3)continent-continent: crust overlaps, little to no subduction, forms high mountains |
| Divergent Plate Boundaries | Extensional force, new crust forms, shallow earth quakes, volcanoes common |
| Mantle Convection | Hot magma rises, cold magma sinks (Arthur Holmes) |
| Continental Drift | All continents were once 1 (pangea) evidence: 1. fit of continents 2. fossils 3. rock type/structures 4. paleoclimate |
| Mechanics of Earth System | lithosphere: solid asthenosphere:plastic mesosphere:solid/plastic outer core: liquid inner core:solid |
| Core | Iron and Nickel |
| Mantle | Ultramafic (Mg, Fe) |
| Crust | oceanic: basalt (mg, Fe) 7-10 km thick continental:Granite (al, k, fe, si) 25-40 km thick |
| Composition of Earth | crust, mantle, core |
| Mineral Properties | Hardness, cleavage, fracture, luster, color, specific gravity, crystals, unique properties |
| Carrying Capacity | maximum # of people earth can hold without causing environmental degradation |
| Science | testable, based on facts and observations not a belief system |