The part of the Earth system comprised of solid (mostly) silicate rock begins at Earth’s ground surface and extends down to the boundary between the mantle and core, about 2890 km below the surface. In a sentence or two, explain which of the three fundamental types of rock (igneous, sedimentary, metamorphic) forms most of the volume of Earth’s crust and mantle. Share your explanation with your classmates. Hint: Look back at Figs. A7.5.4 and A7.5.5, and remember that very little of the volume of the crust or mantle is liquid magma.
The part of the Earth system comprised of solid (mostly) silicate rock begins at Earth’s ground surface and extends down to the boundary between the mantle and core, about 2890 km below the surface. In a sentence or two, explain which of the three fundamental types of rock (igneous, sedimentary, metamorphic) forms most of the volume of Earth’s crust and mantle. Share your explanation with your classmates. Hint: Look back at Figs. A7.5.4 and A7.5.5, and remember that very little of the volume of the crust or mantle is liquid magma.
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
Related questions
Question
The part of the Earth system comprised of solid (mostly) silicate rock begins at Earth’s ground surface and extends down to the boundary between the mantle and core, about 2890 km below the surface. In a sentence or two, explain which of the three fundamental types of rock (igneous, sedimentary, metamorphic) forms most of the volume of Earth’s crust and mantle. Share your explanation with your classmates. Hint: Look back at Figs. A7.5.4 and A7.5.5, and remember that very little of the volume of the crust or mantle is liquid magma.

Transcribed Image Text:Pressure (kilobars)
O
15
0
diagenesis
?
100
zeolite
200
subgreenschist
300
B.
epidote-amphibolite
400
500
Temperature (°C)
600
px-hornfels sa
700
granulite
800
900
0
10
20
30
40
50
Depth (km)

Transcribed Image Text:Subducting
sediments
are metamorphosed
due to increase in
pressure and
temperature.
300°C
600°C
900°C
1200°C
Idealized
geothermal
gradient
Shallow crustal
rocks are
metamorphosed by
heat emanating
from a nearby
magma body.
Subducting oceanic lithosphere
Low geothermal gradients are observed
in subduction zones because cold
oceanic crust and overlying sediments
are descending into the mantle.
Igneous
intrusions
Rocks buried in a
large sedimentary
basin may encounter
low-grade
metamorphic
conditions near the
bottom of the pile.
Rising magma transports heat to
Earth's upper crust causing an
increase in the geothermal
gradient.
Subsiding
basin
300°C
600°C
--900°C
200°C
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