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Journey to the Center: Exploring the Layers of the Earth
Presentation
•
Science
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6th - 8th Grade
•
Practice Problem
•
Medium
+8
Standards-aligned
Jack Granzow
Used 208+ times
FREE Resource
7 Slides • 4 Questions
1
Journey to the Center
Exploring the Layers of the Earth
2
Layers of the Earth
3
Multiple Choice
Which layer of the Earth is composed of solid iron and nickel?
Crust
Mantle
Outer Core
Inner Core
4
Inner Core
The inner core of the Earth is composed of solid iron and nickel. It is the hottest and most dense part of our planet, with temperatures reaching up to 5,500 degrees Celsius. Despite its extreme heat, the immense pressure keeps the inner core solid. It plays a crucial role in generating Earth's magnetic field.
5
Journey to the Center
Heat Transfer in the Mantle (you need to know)
the Layers of the Earth
Understand the Mantle's Role in tectonics
Convection in the mantle
Implications for Earth's Dynamic Changes
6
Multiple Choice
What is the main method of heat transfer in the mantle?
Convection
Radiation
Conduction
Advection
7
Heat Transfer in the Mantle
Trivia: The main method of heat transfer in the mantle is convection. Convection occurs when hot material rises, cools, and then sinks back down. This process creates a continuous cycle of heat transfer, helping to drive the movement of tectonic plates on Earth's surface. Fun Fact: The mantle is the layer between the Earth's crust and core, and it makes up about 84% of the Earth's volume.
8
The Moho: Boundary
The Moho is the boundary between the Earth's crust and mantle.
It was discovered by Andrija Mohorovičić in 1909.
The Moho is characterized by a significant increase in seismic wave velocity.
It separates the rigid crust from the more ductile mantle.
Understanding the Moho helps us study the Earth's structure and tectonic processes.
9
Multiple Choice
Who discovered the Moho?
Andrija Mohorovičić
Albert Einstein
Dwayne Johnson
Alfred Wegener
10
Moho Discovery
Trivia: The Moho, or Mohorovičić discontinuity, was discovered by Andrija Mohorovičić. It is the boundary between the Earth's crust and mantle. This discovery revolutionized our understanding of the Earth's structure. It was discovered using seismic waves in October of 1909.
11
Reorder
Reorder the following layers from the inside of the Earth to the outside.
Inner Core
Outer Core
Mesosphere
Asthenosphere
Cust
Journey to the Center
Exploring the Layers of the Earth
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