Igneous Processes and Products

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Igneous Processes and Products
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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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