Explore Exploration Activity The compositional zones of Earth's interior are the crust, mantle, outer core, and inner core. Each zone has unique physical and structural properties. The crust is the thin, solid, outermost zone of the Earth. It is approximately 35 kilometers thick. Below the crust is the mantle. Earth's mantle is more dense and thicker than the crust. It is approximately 2,900 kilometers thick. The outer core lies beneath the mantle and is hypothesized to be liquid in composition. It is 2,250 kilometers thick. Finally, the inner core is believed to be solid and is 1,250 kilometers thick. Surface 400 km 670 km 1000- Solidus Mantie Sold 2000 - I 3000 - Temperature Met Using the diagram to the right, fill in the temperature values for the depth distances given in the table below. The first row is completed for you as an example. 4000 - Outer Core 5000 - Inner Core 6000 - 1000 2000 3000 4000 5000 Temperature (C) Zone Depth (Kilometers) Temperature ("C) Crust 1 km 25°C Mantle 1,000 km Outer Core 4,000 km 6,000 km Inner Core General Science IA Credit 2 Depth (km)
Explore Exploration Activity The compositional zones of Earth's interior are the crust, mantle, outer core, and inner core. Each zone has unique physical and structural properties. The crust is the thin, solid, outermost zone of the Earth. It is approximately 35 kilometers thick. Below the crust is the mantle. Earth's mantle is more dense and thicker than the crust. It is approximately 2,900 kilometers thick. The outer core lies beneath the mantle and is hypothesized to be liquid in composition. It is 2,250 kilometers thick. Finally, the inner core is believed to be solid and is 1,250 kilometers thick. Surface 400 km 670 km 1000- Solidus Mantie Sold 2000 - I 3000 - Temperature Met Using the diagram to the right, fill in the temperature values for the depth distances given in the table below. The first row is completed for you as an example. 4000 - Outer Core 5000 - Inner Core 6000 - 1000 2000 3000 4000 5000 Temperature (C) Zone Depth (Kilometers) Temperature ("C) Crust 1 km 25°C Mantle 1,000 km Outer Core 4,000 km 6,000 km Inner Core General Science IA Credit 2 Depth (km)
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
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Transcribed Image Text:Explore
Exploration Activity
The compositional zones of Earth's interior are
the crust, mantle, outer core, and inner core.
Each zone has unique physical and structural
properties. The crust is the thin, solid, outermost
zone of the Earth. It is approximately 35
kilometers thick. Below the crust is the mantle.
Earth's mantle is more dense and thicker than the
crust. It is approximately 2,900 kilometers thick.
The outer core lies beneath the mantle and is
hypothesized to be liquid in composition. It is
2,250 kilometers thick. Finally, the inner core is
believed to be solid and is 1,250 kilometers thick.
Surface
400 km
670 km
1000-
Solidus
Mantie
Sold
2000 -
I 3000 -
Temperature
Met
Using the diagram to the right, fill in the
temperature values for the depth distances given in
the table below. The first row is completed for you
as an example.
4000 -
Outer Core
5000 -
Inner Core
6000 -
1000 2000 3000 4000 5000
Temperature (C)
Zone
Depth (Kilometers)
Temperature ("C)
Crust
1 km
25°C
Mantle
1,000 km
Outer Core
4,000 km
6,000 km
Inner Core
General Science IA
Credit 2
Depth (km)
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