esq2 Flashcards
three main sources of heat of the earth
primordial heat, decay of radioactive isotopes, tidal friction
leftover heat from the formation of Earth
primordial heat
comprises the lithosphere
crust and uppermost part of the mantle
below the lithosphere, 180 km and contains thick hot molten rocks or magma
asthenosphere
outermost layer of the earth where life exists
crust
the crust that makes up the continents, and is 40-70km thick
continental crust
below the crust, a semisolid, rocky and very hot layer, 2900km thick, makes up 80% of earth and carries most of its mass.
mantle
composition of the mantle
ferro-magnesium silicate rocks
two distinct layers of the core
outer and inner core
the only layer in the Earth that is liquid, which is made up of molten nickel and iron. about 2270km thick with temperatures ranging from 3700C-4300C.
Outer core
1220km as its diameter, composed of mostly solid iron, extremely hot and about 6000C
Inner core
Boundaries between the layers of the Earth
Conrad discontinuity (upper-lower crust)
Mohorovicic discontinuity (crust-upper mantle)
Repetti discontinuity (Upper mantle-lower mantle)
Gutenberg discontinuity (lower mantle-outer core)
Lehmann discontinuity (outer core-inner core)
places where magma can be formed
mid-oceanic ridges
mantle plumes
subduction zones
hot molten rock containing chemical elements from uppermost mantle called asthenosphere
magma
an extent of a fluid’s resistance to flow
viscosity