Creado por siobhan.quirk
hace más de 11 años
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Pregunta | Respuesta |
Igneous Rocks | those that have cooled from magma |
Magma | molten rock |
Lava | molten rock that cools at the surface |
Silicic igneous rocks | have a composition rich in silica, of more than 66% and are light coloured (leucocratic) |
Intermediate igneous rocks | Have a silica content of 66 to 52% and are grey (mesocratic) |
Mafic igneous rocks | have a silic contnent of less than 45% |
Felsic minerals | light coloured and silica rich |
Mafic minerals | dark coloured, silica poor and rich in magnesium and iron |
Cooling | igneous rocks may be at the surface or the depth |
Extrusive | general term for all igneous rocks that cool at the surface - both lava and pyroclasts |
Intrusive | term for igneous rocks that cool below the surface |
Hypabyssal | igneous rocks form at relatively shallow depths below the surface |
Plutonic | when igneous rocks form deep below the surface |
Divergent plate margin | where two plates are moving apart and magma is rising up between them |
Convergent plate margin | where two plates are colliding and magma is formed above a subduction zone or deep in the crust |
Hot spot | formed by a fixed mantle plume bringing magma to the surface |
Partial melting | occurs where some of the minerals in a rock melt to form a magma |
Country rock | any rock, whether sedimentary, igneous or metamorphic into which an igneous rock is intruded |
Minor intrusions | cool at hypabyssal depth below the surface and include sills and dykes |
Major intrusions | plutonic and cool deep below the surface and include batholiths |
Contact | where igneous rock meets country rock |
Chilled margin | where the igneous rock has cooled rapidly so it has fine crystals |
Baked margin | country rock that was heated and altered by the intrusion |
Metamorphic aureole | large area around a batholith where the rocks have been metamorphosed |
Pyroclast | an individual fragment ejected during an eruption |
Pyroclastic | fragmental materials formed by explosive eruptions, including bombs, blocks, lapilli and ash |
Volcano | a vent at the surface of the Earth through which magma and other volcanic materials are ejected |
Pyroclastic rocks | are formed when the pyroclastic material is compacted into rocks |
Pyroclastic flow | a hot mixture of pyroclastic material and gas. A nuee ardente is a type of pyroclastic flow |
Isopachyte | a line joining points of equal thickness of a deposit such as ash. The maps may be called isopach maps |
Lahars | mudflows of wet ash and volcanic debris that can flow rapidly down a mountainside |
Viscosity | measure of a fluid's resistance to flow and controls the stickiness of a magma, which in turn depends on the silica content |
Shield volcanoes | gentle slopes of less than 10 degrees and a roughly circular shape around a central vent |
Fissure eruptions | where magma reaches the surface along long, linear cracks or fissures |
Submarine eruptions | where magma comes from a vent or fissure on the sea floor |
Low viscosity | where magma is fluid and flows freely |
Effusive | term used to describe the fluid, non-explosive, basalt lava |
Hawaiian eruption | large amounts of very fluid basaltic magma from which gases escape, but few pyroclasts |
Strombolian eruption | more explosive with less fluid basalt and andesite lava. Regular explosions of gas and pyroclastic material |
Vulcanian eruption | violent with viscous andesitic lava and large quantities of pyroclastic material from large explosions |
Plinian eruptions | extremely explosive with viscous as-filled andesitic and rhyolite lava and tremendous volumes of pyroclastic material blasted out |
active | volcano has eruptive activity within recorded history. Currently there are about 600 active volcanoes and each year 50 to 60 actually erupt |
extinct | volcano has not shown any historic activity and is usually deeply eroded |
dormant | volcano is one that has not shown eruptive activity within recorded history, but shows geological evidence of activity within the geologically recent past |
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