The document discusses evidence for tectonic plate movement. Similar fossils and rock types found on opposite sides of oceans provided early evidence. Today, plate boundaries are identified by the locations of volcanoes and earthquakes. Volcanoes result from the friction of plate movement, while earthquakes occur where plates rub against each other. Seafloor ages also provide evidence, as ages get younger approaching mid-ocean ridges. Plate types - oceanic and continental - and effects of plate tectonics such as seafloor spreading, volcanoes, earthquakes, and mountain formation are also outlined.

1. Tectonic plates

2. Tectonic Plates
Our first evidence of tectonic motion is based on similar fossils and
rock types on opposing sides of the ocean

3. Tectonic Plates

4. Tectonic Plates
Today plate boundaries are determined by examining
the location of volcanoes and earthquakes.
Volcanoes result from the friction (heat) of the plates
motion.
Earthquakes occur where plate rub against one another

5. Tectonic Plates

6. Tectonic Plates
Volcanoes

7. Tectonic Plates

8. Tectonic Plates

9. Tectonic Plates

10. Tectonic Plates-
oceanic ridge

11. Tectonic Plates
Another source of
evidence is based
on seafloor ages
which get younger
as we approach
sea floor ridges

12. Plate Types
• Oceanic plates: basalt
– Dark (black) and dense rock
type composed of
silicates, iron and magnesium
• Continental plates – granite
and andesite
– Light colored (pink, white and
gray) and low density rock
type composed almost
entirely of silicates.

13. The movement of the
tectonic plates cause:
• SEAFLOOR SPREADING.
• VOLCANOES
• EARTHQUAKES
• MOUNTAIN FORMATION
• MOVEMENT OF CONTINENTS