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Description of the Earth

      Shape and size
         Layers
       Movements
The Earth
•Is the third planet of the solar system
•Is the sixth largest planet of the solar system


The Earth is not a perfect sphere
•The equator circumference is about 24,901.55 miles
•The north pole is dilated 10 meters
•The equator is 27km wide.
The Earths        Orbit:     The
circumference of the orbit is
approximately 938,900,000. The
Earth    travels    along    this
circumference    at a speed of
106,000 kilometers per hour.
The Earths rotation
Rotates on its axis
It takes 24 hours.
Stratigraphy, in geology, the study of rock
layers, or strata, particularly their ages,
compositions, and relationships to other
rock layers. Stratigraphy provides
geologists with clues about the earth’s
past. Stratigraphy also allows geologists to
predict what types of rocks lie below the
ground and to understand geologic
processes. Consequently, most geologists
regularly use basic elements of
stratigraphy in their work.



                                               n
Origins of Earthquakes
Origins of Volcanic Eruptions

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The earth

  • 1. Description of the Earth Shape and size Layers Movements
  • 2. The Earth •Is the third planet of the solar system •Is the sixth largest planet of the solar system The Earth is not a perfect sphere •The equator circumference is about 24,901.55 miles •The north pole is dilated 10 meters •The equator is 27km wide.
  • 3. The Earths Orbit: The circumference of the orbit is approximately 938,900,000. The Earth travels along this circumference at a speed of 106,000 kilometers per hour.
  • 4. The Earths rotation Rotates on its axis It takes 24 hours.
  • 5. Stratigraphy, in geology, the study of rock layers, or strata, particularly their ages, compositions, and relationships to other rock layers. Stratigraphy provides geologists with clues about the earth’s past. Stratigraphy also allows geologists to predict what types of rocks lie below the ground and to understand geologic processes. Consequently, most geologists regularly use basic elements of stratigraphy in their work. n