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Geomorphic region showing in all its parts similar climate and geologic structures and having relief features readily differentiated from those of neighboring regions. |
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Combinations of landforms |
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Cuts through older rock (igneous) |
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rock unit containing one or more beds with distinctive physical and chemical characteristics |
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two or more geographically associated formations with notable common features |
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Minor rock unit within a formation |
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Squeezed between rock layers |
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surface fractures, or partings, in rock without displacement. |
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sequence of crisscross, dipping beds deposited by water or wind currents of variable direction |
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large curved sheets or slabs of rock peel off from a bedrock surface; caused by physical and chem forces |
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moisture in cracks and joints freeze ad expand |
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Oxygen uniting with another element |
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process of weathering; downward trickling or running water not confined by a channel |
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dissolving of soluble minerals in rock |
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physical and chem process that has effect of rounding off pinnacles and knobs |
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narrow sandstone ridges that are eroding along parallel joints |
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similar to fins but have more crisscross fractures |
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zones where the plates split and spread apart |
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Convergent Plate Boundary |
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zones where plates collide |
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zone where plates slide horizontally past each other |
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Plates are too light to subduct, so they converge and from large mountain ranges |
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Three layers of Earth (Composition) |
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Crust- thin layer covers exterior Mantle- 80% volume of earth Core- metal and mostly nickel and iron |
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Five layers of Earth (Physical) |
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Lithosphere- Upper most mantle+ crust Asthenosphere-upper mantle, plastic rock Mesosphere-middle and lower mantle Outer Core- liquid metal Inner Core-solid metal |
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Five Major geological consequences of subduction |
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-trenches -chain of volcanoes -Earthquakes -Constant plate destruction - young sea floors -mountain ranges form |
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pieces of crust that formed in one location, but later transported by moving plates |
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How do terranes become accreted to a continental margin? |
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They can become "glued" if they are too light to subduct |
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Three basic families and the differences |
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Igneous- formed from cooling and consolidation of magma
Sedimentary- formed from particles of broken down rocks
Metamorphic- changed form in the solid state due to heat, pressure and chem alteration |
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Differences (color, silica content, and grain size) between granite and basalt |
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Granite is lighter, higher silica content and coarse grained |
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Differences (color, silica content, and grain size) between basalt and rhyolite |
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Basalt has less silica, is darker and both are fine grained |
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What are the coarse grained equivalents rocks to rhyolite, andesite and basalt |
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Granite- Diorite - Gabbro |
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volcanic rock ejected during an eruption EX: pumice, volcanic ash, cinders, volcanic breccia |
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large igneous intrusions composed of granite-like rocks |
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viscous, slow-moving, little gas, angular blocks |
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fluid, faster-moving, lots of gas, surface smooth or rope-like |
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Four major processes of forming clastic rocks |
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weathering- physical and chem breakdown of rock Erosion-picking up and transporting weathered products Deposition- settling of sediment Compaction/cementation- |
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fine-grained; microscopic particles of clay minerals, quartz, and mica |
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mainly mineral calcite, may be crystalline |
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composed rounded rock fragments and harder rock |
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high-grade; composition similar to granite; alternating bands of light and dark minerals |
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minerals are strongly aligned and large enough to see |
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fine-grianed; harder and more brittle than shale; splits into flat sheets |
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Three principle causes of metamorphism |
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heat, pressure and chemical alteration |
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Eras of the Phanerozoic Eon (oldest to youngest) |
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Paleozoic, Mesozoic, Cenozoic |
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Periods of Paleozoic Era (oldest to youngest) |
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Cambrian, Ordovician, Silurian, Devonian, Mississippian, Pennsylvanian, Permian |
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Periods of Mesozoic Era (oldest to youngest) |
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Triassic, Jurassic, Cretaceous |
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Periods and Epochs of Cenozoic Era |
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Periods- Tertiary, Quaternary Epochs- Paleocene, Eocene, Oligocene, Micocene, Pilocene, Pleistocene, Holocene |
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