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54 Cards in this Set

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Mineral

solid inorganic substance of natural occurence

streak

powdered form of mineral

fracture

breaks along irregular boundaries (smooth, curved edges)

Mohs' hardness scale

a numerical value of hardness 1 (softest; talc) 10 (hardest; diamond)

Silicates

any one of numerous minerals that have the silicon-oxygen tetrahedron as their basic structure

silica-oxygen tetrahedron

silicon atom with four surrounding oxygen atoms arranged to define the corners of a tetrahedron; basic building blocks of silicates

Pyroclastic

Pyro=fire; clastic=broken

Intrusive

crystallizes inside the crust from magma

Extrusive

crystallizes outside the crust from lava

Aphanitic

Microscopic crystals-not visible

Ultramafic

Lowest silica, Fe and Mg rich

Felsic

highest silica, quartz and feldspar rich

fractional crystallization

magma changes composition continually

pyroclasts

fragments of lava that fall to the ground after volcanic explosions, smaller bits travel farther

Volcanic Ash

smallest bits: fine, light colored

fissure

a crack in rock along which there is a distinct separation

volcanic dome

form of viscous felsic lavas, steep-sided and small, grow slowly

stratovolcano

-mainly alternating pyroclastic deposits and andesitic lava flows


-slopes are intermediate in steepness


-large


-intermittent eruptions over long time span


-eruptions often highly explosive

Andesitic lava

intermediate in composition and viscosity between mafic and felsic magmas

Bond types

-Ionic


-Covalent


-Metallic

Hardness

resistance to scratching

cleavage

breaks along definite planes of weakness (straight edges)

Index minerals

-talc (softest)


-gypsum


-calcite


-fluorite


-apatite


-feldspar


-quartz


-topaz


-corundum


-Diamond (hardest)

Sialic

light colored with silicon and aluminum

chemical bonds

form mineral compounds

composition

what minerals the rock contains

magma/lava

magma-underground


lava-above ground

Phaneritic

crystals visible with the naked eye

mafic

low silica

decompression melting

melting at divergent plate boundaries and hot spots

pegmatite

very coarse-grained igneous rock (typically granite) commonly found as a dike associated with a large mass of plutonic rock that has smaller crystals. large crystals

lahars

water, gas & pyroclastic debris

volcanic bombs

rounded fragments of ejected magma

crater

depression at the summit of a volcano or a depression that is produced by a meteorite impact

shield volcano

-formed mainly of basltic lavas


-gentle sides


-huge; wide


-long duration of activity


-non-violent eruptions

basaltic lava

low-viscosity mafic lavas, typically erupt at 1000-1200 degrees C

Viscosity

resistance to flow

color

how mineral interacts with light

luster

how mineral scatters light

cleavage types

-basal: one direction


-prismatic: two directions at right/non-right angles


-cubic-three directions at right angles


-rhombohedral-three directions at non-right angles


-octahedral-four directions

mineral classification

silicates vs. nonsilicates

Ferromagnesium

darker with more iron (Fe) and magnesium

texture

size & shape of the minerals; look & feel of the rock

glassy

no crystals

porphyitic

two sizes of crystals

intermediate

moderate silica

flux melting

adding water-melting at convergent plate boundaries:addition of water as wet ocean crust is subducted

types of basalt flows

-flood: thick widespread accumulations of basalt, typically fed by fissures


-pahoehoe: low viscosity basaltic lava with ropy texture


-Aa: low viscosity basaltic lava characterized with jagged, blocky texture


-pillow: forms beneath the water, characterized by glassy pillows filled with crystalline basalt


-vesicular: trapped gases form bubbles (vesicles)

pyroclastic flow

gas & pyroclastic debris

lapilli

little stones: dark lapilli-cinders or scoria; light lapilli-pumice

caldera

large depression; formed by collapse of a volcano into a partially drained magma

magma chamber

large underground pool of liquid rock beneath the surface of the earth

Cinder-cone volcano

-formed mainly of basaltic pyroclastic material


-steep sides


-relatively small


-short-lived: typically a single event

rhyolitic lava

High-viscosity felsic lavas, typically erupt at 800-1200 degrees C; most explosive