Table of Contents
What are the physical properties of the mantle?
It is mostly solid rock, but less viscous at tectonic plate boundaries and mantle plumes. Mantle rocks there are soft and able to move plastically (over the course of millions of years) at great depth and pressure. The transfer of heat and material in the mantle helps determine the landscape of Earth.
What are the physical and chemical properties of continental crust?
Continental crust is broadly granitic in composition and, with a density of about 2.7 grams per cubic cm, is somewhat lighter than oceanic crust, which is basaltic (i.e., richer in iron and magnesium than granite) in composition and has a density of about 2.9 to 3 grams per cubic cm.
Which two describe properties of Earth’s crust?
The crust of the Earth is composed of a great variety of igneous, metamorphic, and sedimentary rocks. The crust is underlain by the mantle. The upper part of the mantle is composed mostly of peridotite, a rock denser than rocks common in the overlying crust. Earth’s crust occupies less than 1% of Earth’s volume.
What is the definition of crust in science?
“Crust” describes the outermost shell of a terrestrial planet. Earth’s crust is generally divided into older, thicker continental crust and younger, denser oceanic crust. The dynamic geology of Earth’s crust is informed by plate tectonics. The crust is made of solid rocks and minerals.
Is the crust a physical layer of the Earth?
1: The layers of the Earth. Physical layers include the lithosphere and asthenosphere; chemical layers are crust, mantle, and core.
What is the average thickness of the Earth’s crust?
The average thickness of the crust is about 15 km (9 mi) to 20 km (12 mi). Because both continental and oceanic crust are less dense than the mantle below, both types of crust “float” on the mantle.
What is this monograph about the Earth’s crust based on?
This monograph is based on the proceedings of a Symposium on the Structure and Physical Properties of the Earth’s Crust, held July 27 through 31, 1970, at the … Show all Please select some articles/chapters to export citations.
What is the difference between the Earth’s crust and the mantle?
Beneath the crust is the mantle, which is also mostly solid rocks and minerals, but punctuated by malleable areas of semi-solid magma. At the center of the Earth is a hot, dense metal core . Earth’s layers constantly interact with each other, and the crust and upper portion of the mantle are part of a single geologic unit called the lithosphere.
What is the relationship between the lithosphere and the crust?
The lithosphere is broken into tectonic plates whose motion allows heat to escape from the interior of the Earth into space. The crust lies on top of the mantle, a configuration that is stable because the upper mantle is made of peridotite and so is significantly more dense than the crust.