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Glossary
A-GH-PQ-Z
ArchaeaBacteria (single-celled organisms) that live at high temperatures such as the high temperatures found within hydrothermal vent structures.
autotrophAn organism that can get energy directly from sunlight through the process of photosynthesis.
bathymetryDepth from the sea surface to the seafloor.
black smokerA chimneylike structure made up of sulfur-bearing minerals that actively bellow black smoke.
buoyancyThe tendency for less-dense material to rise.
chemosynthesisThe process of using chemical energy to create food.
chemotrophAn organism that gets energy from the oxidation of chemicals. At deep-sea hydrothermal vents, the chemotrophs oxidize hydrogen sulfide in the water that discharges from black smokers.
clay mineralA hydrous mineral formed by interaction between a hydrothermal solution and a mineral such as feldspar, mica, pyroxene, etc.
collapsed lava pitsFeatures created when the tops of lava tubes collapse inward.
coreThe spherical mass, consisting largely of metallic iron, at the center of Earth. The radius of the core is approximately 3,000 kilometers.
crustThe outermost and thinnest of Earth's compositional layers, the crust consists of rocky material that is less dense than the rocks of the mantle below. The continents make up the continental crust, and the crust beneath the oceans is the oceanic crust. The oceanic crust varies in thickness from 6 to 8 kilometers, and the continental crust varies in thickness from 30 to 70 kilometers.
crystalline rockRock consisting of minerals in an obviously crystalline state. Often used to refer to slowly cooled igneous rocks.
crystallizationThe process through which minerals grow from a liquid.
dikesThin, tabular, parallel-sided sheets of intrusive igneous rocks that generally cut across existing rock layers in a roughly vertical fashion.
earthquakeA sudden motion or tembling in the earth caused by the rapid breaking of rocks along faults.
ecosystemA group of organisms and their habitat.
faultA fracture in a rock along which movement occurs or has occurred.
fissuresOpen cracks such as those that form in the oceanic crust due to plate separation.
fracture zonesValleys on the ocean floor that run perpendicular to ocean ridges, separating offset segments of the ridge. Fracture zones are bound by both strike-slip faults and normal faults. Rocks from the deep oceanic crust are often exposed by these faults.
hydrothermalAn adjective applied to heated or hot-water-rich solutions.
hydrousAn adjective applied to water-bearing substances.
igneous mineralA mineral that forms when magma or lava solidifies.
lavaMolten rock that erupts onto Earth's surface.
lystric faultA fault with a curved fault surface. Many of the normal faults along the ocean ridges are lystric. They penetrate down into the crystalline rock of the oceanic crust.
magmaMolten rock under Earth's surface.
mantleThe thick shell of dense, rocky material that surrounds the core and lies beneath Earth's crust. The mantle is approximately 2,800 kilometers thick.
mid-ocean ridgeA 50,000 km submarine mountain range along which oceanic plates are formed.
mineralAny naturally formed crystalline solid with a definite chemical composition and a characteristic crystal structure.
ocean basinThe ocean floor that includes the submerged plains and ocean ridges.
oceanic crustThe crust beneath the oceans.
oreAn aggregate of minerals from which one or more minerals can be extracted for profit.
photosynthesisThe process of using sunlight to create food.
pillow lavasRounded pieces of basaltic lava that are created when the lava erupts under water.
platesThe rigid pieces that make up the puzzle of Earth's crust.
precipitationThe separation of minerals from a liquid or gas.
reactivityThe tendency for one substance to dissovle another substance.
ROVRemotely operated vehicle, in this case a remotely operated submersible.
sessileThe tendencey to stay in one place.
sheet flowsThin, flat flows similar to those that are found on Hawaii.
solutionA liquid combination of a liquid and a nonliquid substance.
spreadingThe separation of plates such as the spreading that occurs along midocean ridges.
subductionPlunging of oceanic plates along trenches either within the oceans or along their boundary with the continents.
submersibleResearch vessel designed to dive beneath the ocean surface. Deep-sea submersibles are designed to go to depths greater than ordinary submarines (depths greater than 2,000 meters).
sulfatesOxygen-rich sulfur-bearing minerals.
sulfide moundsLarge piles of sulfide minerals built up over time.
sulfidesOxygen-poor sulfur-bearing minerals.
symbiontsUsually refers to at least two organisms that need each other to survive, with one organism living within the other organism.
tectonicA term designating rock structures and external forms resulting from the deformation of Earth's crust.
thermophyllicHeat loving.
topographyVariation in altitude of the landscape.
zero-ageOceanic crust formed with the last 10,000 years.

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