Final (Chapter 13-20) Flashcards
(176 cards)
why do continents rise above oceans?
isostasy
what is isostasy?
buoyant continental lithosphere floats on dense asthenosphere
what is orogenesis?
mountain-building processes
what are the 3 plate boundaries?
divergent, passive, convergent
what are divergent continental margins?
mantle plume rises, uplifts and splits continental lithosphere to form rift valley with blocks dropped along normal faults, and volcanoes along valley sides

what are passive continental margins?
rift widens, seawater invades, and a new ocean basin forms whose sides experience no seismic activity but gradually subside under weight of sediment load

what are convergent continental margins? (2 types)
as mountains grow, undergo isostatic adjustments to balance weight
what are andean-type convergent margins?
oceanic crust subducts beneath continental, developing accretionary wedge, continental volcanic arc, and plutons in core of deformed mountain belt

what are aleutian-type convergent margins?
oceanic crust subducts under oceanic, to form volcanic island arc

what is continental collision? (convergent margins)
ocean basin closes, subduction stops, highest mountains form (continental crust cannot subduct under more continental crust therefore creates very high mountain *push eachother up*)

what are accreted terranes? (convergent margins)
foreign pieces of crust forefully attached to continental margin

what is the Wilson cycle?
oceans opened and closed, mountains built and rebuilt repeatedly; rarely pieces of oceanic crust got stuck onto continental margin during obduction
what is uplift? (broad vertical movements in continents)
by mantle upwelling pushing up continental lithosphere in continent interiors
what is subsidence?
how is it caused?
gradual sinking in or land
mainly due to weight of sediment deposited along passive continental margins as mountain belt erodes; also downward mantle flow pulling on lithosphere

what is the origin and evolution of continental crust?
formed by the combining of volcanic arcs above subduction zones
where is the earliest continental crust found today?
in shield areas of continental interiors
what is the main trigger of mass wasting? and what intensifies this trigger?
gravity: always pulling rock, regolith and soil down slopes….more effective if water saturates materials on slopes, reduces cohesion friction and adds weight

what causes oversteepened slopes?
due to undercutting by waves, streams, and human excavation, resulting in loss of support for materials higher up in the slope

how does removing vegetation trigger mass wasting?
vegetation anchors soil and regolith with plant roots; removing plants make the slope unstable and susceptible to failure

how do earthquakes trigger mass wasting?
can dislodge rock and unconsolidated material, resulting in landslides
how is mass wasting classified?
based on types of materials, types of motion (freefall, sliding and flowing) and how fast they move
what is slump mass wasting?
rotation of a block of slope material along a sliding surface (usually lubricated by water) gravity pulls the block in a rotational motion away from a scarp with the block’s surface tilting back - happens when they slop is undercut by a stream, by waves or by human excavation

what is rockslide mass wasting?
common where rock structures parrallel slopes (mountainous areas) provide sliding surface, or where stronger rock rests on weaker rock especially if the slope is undercut, sliding surface is lubricated after heavy rain or snowmelt, or shaken by an earthquake

what is debris flow?
fast flow of saturated soil and regolith down valleys following heavy rain OR during and after volcanic eruptions where ash gets mixed with melted snow and ice rushing down valleys (lahars)






























