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PHOTOGRAPHIC
   EVIDENCE
Gladys Torres
Earth Science
March 2012
Class L
CONVERGENT BOUNDARY
CONVERGENT BOUNDARY
 Convergent Boundaries are plates coming together.
  There are three different types of Convergent
  Boundaries. Ocean-Ocean forms arcs of islands and
  strato volcanoes. Ocean-Continent forms volcanoes and
  mountain ranges. Continent-Continent forms huge
  mountain ranges like the Himalayas in Nepal.
DIVERGENT BOUNDARY
DIVERGENT BOUNDARY

Divergent Boundaries are plates pulling apart.
 When Plates diverge, the Earth’s crust splits
 apart causing magma to rise from the
 mantle, depending if it happens at sea or
 land, it forms mid-ocean ridges or rift valleys.
TRANSFORM BOUNDARY
TRANSFORM BOUNDARY

Transform Boundaries are plates slidding past
 each other. This boundary releases a cause of
 a violent earthquake. The min types of waves
 are, P waves, waves that go back and forth. S
 waves, waves that go up and down and L
 waves, waves that go in all directions and the
 most dangerous.
FAULT ZONE
SUBDUCTION ZONE
FAULT AND SUBDUCTION ZONE

A subduction zone is when one plate goes
 under another. An oceanic plate goes down
 because is more dense (heavier) and the
 continental plate goes up because is lighter.
 This happens because of faults, causing the
 formation of trenches and volcanoes.
EARTHQUAKE
TSUNAMI
EARTHQUAKE AND TSUNAMI

An Earthquake is formed by Transform plate
 boundary. The earthquakes first movement
 happens in the focus and the epicenter is the
 point on Earth’s surface above the focus and
 plates move. Earthquakes happen on land.
 Thrust/Reverse Fault causes an upward wave
 or a Tsunami. A tsunami is an underwater
 earthquake, landslide, or a volcanic eruption.
HOT SPOT
HOT SPOT

Hot Spots are areas of volcanic activity from
 deep under the Earth’s mantle. An example of
 a hot spot is Hawaii, an island made up of
 volcanoes that are no longer active.

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Photographic Evidence of Plate Boundaries

  • 1. PHOTOGRAPHIC EVIDENCE Gladys Torres Earth Science March 2012 Class L
  • 3. CONVERGENT BOUNDARY  Convergent Boundaries are plates coming together. There are three different types of Convergent Boundaries. Ocean-Ocean forms arcs of islands and strato volcanoes. Ocean-Continent forms volcanoes and mountain ranges. Continent-Continent forms huge mountain ranges like the Himalayas in Nepal.
  • 5. DIVERGENT BOUNDARY Divergent Boundaries are plates pulling apart. When Plates diverge, the Earth’s crust splits apart causing magma to rise from the mantle, depending if it happens at sea or land, it forms mid-ocean ridges or rift valleys.
  • 7. TRANSFORM BOUNDARY Transform Boundaries are plates slidding past each other. This boundary releases a cause of a violent earthquake. The min types of waves are, P waves, waves that go back and forth. S waves, waves that go up and down and L waves, waves that go in all directions and the most dangerous.
  • 10. FAULT AND SUBDUCTION ZONE A subduction zone is when one plate goes under another. An oceanic plate goes down because is more dense (heavier) and the continental plate goes up because is lighter. This happens because of faults, causing the formation of trenches and volcanoes.
  • 13. EARTHQUAKE AND TSUNAMI An Earthquake is formed by Transform plate boundary. The earthquakes first movement happens in the focus and the epicenter is the point on Earth’s surface above the focus and plates move. Earthquakes happen on land. Thrust/Reverse Fault causes an upward wave or a Tsunami. A tsunami is an underwater earthquake, landslide, or a volcanic eruption.
  • 15. HOT SPOT Hot Spots are areas of volcanic activity from deep under the Earth’s mantle. An example of a hot spot is Hawaii, an island made up of volcanoes that are no longer active.