exam 2 Flashcards
mantle
a layer inside a planetary body bounded below by a core and above by a crust
crust
thin outer, rocky layer of earth
thicker crust is more elevated than thinner crust
core
the very hot, very dense center of our planet
lithosphere
rigid, relatively cool outermost shell that consists of the crust and the uppermost mantle
- average thickness of 100 km
- more than 250 km thick below oldest portions of continents
asthenosphere
- soft relatively weak layer of the mantle
- temp/pressure conditions are such that rock is near its melting point and is easily deformed
lower mantle
lower relatively more rigid layer of the mantle
- increasing pressure results in increasingly stronger rocks between 660 km and 2900 km
- still some deformation of rocks
outer core
liquid shell of iron nickel alloy that is 2260 km thick
- the flow of metallic iron in this zone generates the earths magnetic field
inner core
solid sphere of iron nickel alloy with a radius of 1216 km
- temperatures high enough to melt iron but the immense pressure compresses it into a solid state
continental crust
the outermost layer of Earth’s lithosphere that makes up the planet’s continents and continental shelves
theory of plate tectonics
- the earths lithosphere is broken into numerous slabs called tectonic plates
- the plates are in continual motion, 2 inches per year
- rigid lithosphere plates move about on the asthenosphere which is softer and capable of gradual flow
oceanic crust
the part of the Earth’s crust that makes up the seafloor
bathymetry
measurement of ocean depths and charting of the ocean floor topography
passive continental margins
are not
associated with tectonic plate boundaries.
Includes the continental shelf, slope and rise.
continental shelf
the gently sloping, submerged perimeter of
a continent.
– Very gentle slope: 2 m per km (0.1 °)
continental slope
a relatively steep structure that
marks the transition from continental to oceanic crust
turbidity currents
gradual incline extending from the base of the continental
slope to the deep-ocean basin
continental rise
gradual incline extending from the base of the continental
slope to the deep-ocean basin.
active continental margins
areas where oceanic
lithosphere is being subducted beneath the leading edge
of a continent.
deep ocean trenches
Surface expressions of subduction zones are
subduction zone
areas where oceanic lithosphere is descending
(being subducted) into the underlying asthenosphere
volcanic arcs
arc-shaped chain of volcanoes that forms
adjacent to a subduction zone.
hotspot
areas of volcanism and high heat
flow associated with a rising plume of hot
mantle material
accretionary wedge
sediments and pieces of oceanic crust
scraped from descending plate and plastered against edge of
the overriding continent
how guyots and atolls form
seamounts
divergent plate boundaries are located
plates pulling apart=