"The Internal Structure of the Earth" The Unquiet Earth PPT Courseware 2

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"The Internal Structure of the Earth" The Unquiet Earth PPT Courseware 2

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"The Internal Structure of the Earth" The Unquiet Earth PPT Courseware 2

learning target

1. Be able to infer the internal structure of the earth based on some natural phenomena.

2. Be able to make a model of the earth's structure.

3. Know the internal structure of the earth.

This is a picture of Earth's Antarctica, stitched together from multiple photos taken by the Galileo spacecraft.

This is a photo of the Earth sent back by the Galileo Jupiter probe on December 11, 1990, when it was 1.5 million miles away from the Earth. The Indian subcontinent and Australia are visible in the picture

This is a photo of the Earth and the Moon taken by the Galileo spacecraft on its way to Jupiter in 1992.

Little knowledge about the earth

The Earth is the third planet from the sun, counting from the inside out, and is about 150 million kilometers away from the sun. The earth orbits the sun once every 365 days and rotates once every 23.9 hours. Its diameter is about 12,756 kilometers, just over a hundred kilometers larger than Venus. People dream of traveling in space and admiring the wonders of the universe. And in a sense, we are all space travelers. Our spaceship is the Earth, flying at a speed of 108,000 kilometers per hour.

How do humans understand the structure of the earth's crust?

Scientists have finally found a way to use seismic waves to uncover the mysteries of the Earth's depths. It turns out that huge earthquakes will shake the earth, sending out sound waves like a giant hammer hitting copper. This sound wave has echoes and bends. When it encounters different materials underground, it will emit different tones.

In 1910, former Yugoslavian seismologist Mohorovich accidentally discovered that seismic waves were refracted 50 kilometers underground. He believed that this zone where refraction occurs is the interface between the earth's crust and different materials below the earth's crust. In 1914, German seismologist Gutenberg discovered that there was another interface between different materials 2,900 kilometers underground. Later, in order to commemorate them, people named the two surfaces "Moho surface" and "Gutenberg surface" respectively. Based on these two surfaces, the earth was divided into three layers: crust, mantle and core.

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For more information about the PPT courseware "Unquiet Earth and the Internal Structure of the Earth", please click the "Unquiet Earth ppt Internal Structure of the Earth" ppt tag.

"The Internal Structure of the Earth" Unquiet Earth PPT Courseware 4:

"The Internal Structure of the Earth" Unquiet Earth PPT Courseware 4 Moho The Moho is located at a depth of 30-40km below the surface. After reaching this interface, the average speed of longitudinal waves suddenly rises from 6-7km/s to 8.1km/s , this mutation is global. This was done by scholars from the former Yugoslavia..

"The Internal Structure of the Earth" Unquiet Earth PPT Courseware 3:

"The Internal Structure of the Earth" Unquiet Earth PPT Courseware 3 Guess the three boxes A, B and C contain different items. How can you guess what's in the box without opening it? Weigh the weight, listen to the sound, smell the smell. It seems that I...

"The Internal Structure of the Earth" Unquiet Earth PPT courseware:

"The Internal Structure of the Earth" Unquiet Earth PPT courseware Import new lesson 1. Explore the dark box: There are three boxes on the table, containing water, fine sand and small stones. 2. How can you guess what’s in the box without opening it? Student exchange with...

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Update Time: 2024-07-24

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"The Internal Structure of the Earth" The Unquiet Earth PPT Courseware 2
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