asthenosphere
The relationship between the inner core outer core-mantle lithosphere and asthenosphere is that the coolest layers are farthest from the core.
its hot but solid rock
A solid lower part and a liquid upper part
The mantle is hotter by a few degrees."The inner core and crust are solid; the outer core and mantle layers are plastic or semi-fluid. The various layers are separated by discontinuities which are evident in SEISMIC DATA; the best known of these is the Mohorovicic discontinuity between the crust and upper mantle." "The core is probably composed mostly of iron (or nickel/iron) though it is possible that some lighter elements may be present, too. Temperatures at the center of the core may be as high as 7500 K, hotter than the surface of the Sun. The lower mantle is probably mostly silicon, magnesium and oxygen with some iron, calcium and aluminum. The upper mantle is mostly olivene and pyroxene (iron/magnesium silicates), calcium and aluminum. We know most of this only from SEISMIC TECHNIQUES; samples from the upper mantle arrive at the surface as lava from VOLCANOES but the majority of the Earth is inaccessible. The crust is primarily quartz (silicon dioxide) and other silicates like feldspar."
The word 'cool' best characterizes the lower mantle.
The relationship between the inner core outer core-mantle lithosphere and asthenosphere is that the coolest layers are farthest from the core.
Medial Malleolus is the best term that describes the inner aspect of the ankle
its hot but solid rock
mantle
No. It best describes the outer core. The inner core is made up of solid iron.
Mechanoreceptors
The epidermis covers the lower and upper sides of the leaf.
Inner ear
A solid lower part and a liquid upper part
The mantle is hotter by a few degrees."The inner core and crust are solid; the outer core and mantle layers are plastic or semi-fluid. The various layers are separated by discontinuities which are evident in SEISMIC DATA; the best known of these is the Mohorovicic discontinuity between the crust and upper mantle." "The core is probably composed mostly of iron (or nickel/iron) though it is possible that some lighter elements may be present, too. Temperatures at the center of the core may be as high as 7500 K, hotter than the surface of the Sun. The lower mantle is probably mostly silicon, magnesium and oxygen with some iron, calcium and aluminum. The upper mantle is mostly olivene and pyroxene (iron/magnesium silicates), calcium and aluminum. We know most of this only from SEISMIC TECHNIQUES; samples from the upper mantle arrive at the surface as lava from VOLCANOES but the majority of the Earth is inaccessible. The crust is primarily quartz (silicon dioxide) and other silicates like feldspar."
it would be an egg. though an egg is oblong, we can tell where the inner core, outer core, mantle, and crust would be.
The word 'cool' best characterizes the lower mantle.