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Published byKatharine Gaunt Modified over 9 years ago
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Landform Geography Earth’s Internal Structure, Rock Cycle, and Geologic Time
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Earth’s Inner Structure Major Layers (outside-in): Lithosphere Upper Mantle Lower Mantle Outer Core Inner Core
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Earth’s Interior
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Lithosphere
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The vast give-and-take at the Earth- atmosphere-ocean interface or cycling within the lithosphere –Fueled by the sun and Earth’s internal heat –Hydrologic Cycle –Rock Cycle –Tectonic Cycle The Geologic Cycle
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Rock Cycle –Rock – assemblage of minerals bound together or a mass of a single mineral… –Minerals – inorganic, nonliving, natural compound having a chemical formula and crystalline structure
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Igneous Rock Formed from cooled magma – liquid rock from asthenosphere Extrusive igneous rock – Intrusive igneous rock – Hypabyssal igneous rock -
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Sources of Igneous Rock
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Extrusive Igneous Rock Basalt - fine-grained, dark-colored extrusive igneous rock Rhyolite - fine- grained, dark-colored extrusive igneous rock
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Intrusive Igneous Rocks Diorite – coarse-grained, intrusive igneous rock Gabbro – coarse-grained, intrusive igneous rock Granite – coarse-grained, intrusive igneous rock
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Sedimentary Rock Vast amts of formerly loose minerals (sediment) deposited in layers Sediments cement to each other in process called lithification – 3 Types:
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Clastic Sedimentary Rock Examples Siltstone Sandstone
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Chemical Sedimentary Rock Formation Andros Island, Bahamas
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Chemical Sedimentary Rock Examples Limestone - can also form chemically from the precipitation of calcium carbonate from lake or ocean water Rock Salt - forms from the evaporation of ocean or saline lake waters.
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Organic Sedimentary Rocks Coal – from plant and organic matter deposited in cool wetlands, forming peat – over time overlying layers of sediment compress & heat peat into coal “Overcooked” deposits become petroleum Natural gas – from microscopic plants at surface of sea water – decompose to gas
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Metamorphic Rocks From igneous & sedimentary rock under great heat & pressure for millions of years Examples of igneous & sedimentary rocks becoming metamorphic: –Shale → Slate → Schist –Limestone → Marble –Sandstone → Quartzite
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Metamorphic Rock Examples Schist Slate Marble Quartzite
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The Rock Cycle
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Geologic Time Earth’s history (4.5 B years) divided into: –Eons Eras –Periods »Epochs Radiometric Dating – compare amt of radio- active isotope to amt of decayed end product in a rock to estimate its age
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Geologic Time
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Geomorphology of Continents and Ocean Basins Geomorphology – study of formation, shape, distribution, & evolution of landforms on Earth Landform – a distinct geographic feature such as a mountain, river valley, coastline, or sand dune Continents consist of 3 basic geomorphic regions: Alpine Chains, Continental Shelves, & Continental Shields
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Continental Shelf Earth’s land area increases dramatically (from 29% to 35% of Earth’s surface) if sea level falls as in a previous glaciation (1.6 my ago) because of the relatively shallow continental shelf.
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Continental Shields Geologically inactive regions with low relief made of old, stable, igneous or metamorphic rock
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Alpine Chains Belts of active mountain building due to volcanic or tectonic processes
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