Term
|
Definition
| scientific study of Earth |
|
|
Term
| Most dangerous geological hazards |
|
Definition
| earthquakes, volcanic eruptions, landslides, floods, and tsunamis |
|
|
Term
|
Definition
| Huge ocean waves, usually caused by displacement of the sea floor |
|
|
Term
|
Definition
| Hot, turbulent mixture of expanding gases and volcanic ash that flows rapidly down the side of a volcano, very deadly |
|
|
Term
|
Definition
| slurry of water and rock debris that flows down a stream channel, very dangerous from a volcanic eruption |
|
|
Term
|
Definition
| an arbitrarily isolated portion of the universe that can be analyzed to see how its components interrelate |
|
|
Term
|
Definition
| includes the atmosphere, hydrosphere, biosphere, and geosphere |
|
|
Term
|
Definition
| the gases that envelop the earth |
|
|
Term
|
Definition
| the water on or near Earth's surface |
|
|
Term
|
Definition
| all the living or once-living material on Earth |
|
|
Term
| Geosphere / solid Earth system |
|
Definition
| the rock and other inorganic Earth material that make up the bulk of the planet |
|
|
Term
|
Definition
| most voluminous of Earth's three major concentric zone, solid rock |
|
|
Term
|
Definition
| thin outer layer of the Earth |
|
|
Term
|
Definition
|
|
Term
|
Definition
| crust and uppermost part of the mantle, relatively rigid and makes up the plates in the plate tectonic theory |
|
|
Term
|
Definition
| uppermost mantle underlying the lithosphere, soft |
|
|
Term
|
Definition
| forces generated inside the Earth that cause the deformation of rock as well as vertical and horizontal movements of portions of the Earth's crust |
|
|
Term
|
Definition
| regards the lithosphere as broken into plates that are in motion that move relative to one another along plate boundaries |
|
|
Term
|
Definition
| two plates that move apart from each other |
|
|
Term
|
Definition
| crests of submarine mountain ranges that usually coincide with divergent boundaries |
|
|
Term
|
Definition
|
|
Term
|
Definition
| rock that forms when magma solidifies |
|
|
Term
|
Definition
| runs along the crest of mid-oceanic ridges |
|
|
Term
|
Definition
| plates moves toward each other |
|
|
Term
| Ocean-continent convergence |
|
Definition
| the oceanicplate is overriden by the less dense continental plate |
|
|
Term
|
Definition
| plate bends beneath another during convergence; occurs with ocean-continent convergence and ocean-ocean convergence |
|
|
Term
|
Definition
| found where oceanic lithosphere bends and begins its descents |
|
|
Term
|
Definition
| rock that forms from high pressure that does not melt but changes state |
|
|
Term
|
Definition
| a type of convergence where two oceanic plates meet, and the less-dense plate is subducted; results in a volcanic island arc |
|
|
Term
|
Definition
| The result of ocean-ocean convergence, such as seen in Indonesia |
|
|
Term
| Continent-continent convergence |
|
Definition
| continental plates buckle and deform with huge vertical uplift and thickening as well as lateral shortening |
|
|
Term
|
Definition
| two plates slide horizontally past each other |
|
|
Term
|
Definition
| vertical movement of sections of Earth's crust to achieve balance |
|
|
Term
|
Definition
| moving water, ice, or wind loosens and removes material |
|
|
Term
|
Definition
| when materials are adjusted to the physical and chemical conditions of their environment so that they do not change or alter with time |
|
|
Term
|
Definition
| product of the breakdown of rock, loose material |
|
|
Term
|
Definition
| loose particles are cemented into this form of rock |
|
|
Term
|
Definition
| to cement loose particles into rock |
|
|