Chapter 15 - Geohazard: Earthquakes and Volcanoes Flashcards
magma
melted rock below the surface of the crust
active volcanoes
volcanoes that have erupted in the past 10,000 years and could erupt again
extinct volcano
volcanoes that have not erupted for tens of thousands of years and will never erupt again
lava
magma that spills into the surface of Earth’s crust
shield volcano
a broad, domed volcano formed from innumerable layers of fluid basaltic lava laid down over tens to hundreds of thousands of years
magma chamber
reservoir of magma beneath a volcano
volcanic vent
the conduit through which magma moves and reaches the surface
volcanic crater
bowl-shaped volcanic depression
flank eruptions
happens where lava pours out the sides of a volcano through side vents, playing an important role in building shield volcanoes
stratovolcano
a large, potentially explosive, cone-shaped volcano composed of alternating layers of lava and pyroclasts; also called composite volcano
pyroclasts
encompasses any fragmented rock material that is ejected from a volcano; fire clasts or pyroclastic materials
ash
pulverized rock particles and solidified droplets of lava that form a fine powder
lava domes
dome-shaped volcanoes that form when thick lava that cannot easily flow piles up around a volcanic vent and solidifies into a domed structure; also called plug domes or volcanic domes
cinder cones
small, cone-shaped volcanoes consisting of pyroclasts that settle at the angle of repose
angle of repose
the steepest angle at with loose sediments can settle, usually ranging between 25 and 35 degrees
mafic lava
lava with a temperature of 1,000-1,200 degrees C and a silica content of 50% or less, resulting in a high viscosity (easy-flowing)
intermediate lava
lava with a temperature of 800-1,000 degrees C and a silica content between 50% and 70%, resulting in a medium viscosity
felsic lava
lava with a temperature of 650-800 degrees C and a silica content of 70% or higher, resulting in a low viscosity (difficult-flowing)
lapilli
rounded marble-to-golf ball-sized fragments of lava that solidify while airborne
pumice
a lightweight, porous rock with at least 50% air content
lava bomb
a streamlined or spherical fragment of lava ejected from a volcano that cools and hardens as it is moving through the air
volcanic block
a fragment of rock that is torn from the volcano’s cone and ejected during an explosive eruption
joints
cracks and weak planes in the rock
columnar jointing
a geometric pattern formed when angular columns result from joint formation in the lava during cooling
large igneous provinces (LIPs)
accumulations of basaltic lava that cover extensive geographic areas
caldera
a large circular depression caused by the collapse of an emptied magma chamber after a volcanic eruption
effusive eruptions
nonexplosive eruptions
explosive eruptions
large volcanic eruptions
volcanic explosivity index (VEI)
system that ranks volcanic eruption magnitude based on the amount of material a volcano ejects during an eruption (scale of 1-8)
lahar
a mudflow that results when a snow-capped stratovolcano erupts, moving a thick slurry of mud, ash, and other debris rapidly down the volcano’s flank
pyroclastic flows
quick-moving avalanches of gas and ash
normal fault
a result of tensional force (extension) as two pieces of Earth’s crust are pulled apart
reverse fault
a result of compressional force that pushes on block upward in relation to another block
fault scarp
a result of the vertical movement of the fault blocks; also called cliff face
focus
hypocenter; the location of initial crust movement along a fault during an earthquake
epicenter
the location on the ground’s surface immediately above the focus and is usually the area of greatest shaking
foreshock
a small earthquake that precedes a larger, main earthquake
aftershocks
small earthquake that follows the shock of a large one
seismographs
instruments used to detect, measure, and record ground shaking; also called seismometers
modified mercalli intensity (MMI) scale
a scale that subjectively ranks the intensity of an earthquake based on structural damage (scale of I to XII)
liquefaction
the transformation of solid sediments into an unstable slurry by ground shaking
moment magnitude scale
an earthquake-ranking system based on the amount of ground movement produced