Title: Oceanic Hot Spots
1 Oceanic Hot Spots
2(No Transcript)
3A Chain of Volcanoes is created by the moving
plate
- The hotspot stays in one place while the plate
moves over it - Click here for a visualization
4Examples of Lava Flows on Kilauea
5Magma Type? Silica? Explosive?
Magma Formation
Lava
Landform
Plate Tectonics
Where on Earth
Basaltic
LOW
Rarely
Increase in temperature
Flows Pahoehoe, Aa, Pillow
Shield Volcano, Chain of Islands
Does not occur at a plate boundary
Hawaii, Iceland
6Continental Hot Spots
7(No Transcript)
8Yellowstone
- About 600,000 years ago
- HUGE volcanic eruptions occurred in Yellowstone,
emptying a large underground magma chamber. - Volcanic debris spread for thousands of square
miles in a matter of minutes. - The roof of this chamber collapsed, forming a
giant smoldering pit. - This caldera was 30 miles (45 km) across, 45
miles (75 km) long, and several thousand feet
deep. - Eventually the caldera was filled with lava.
9 10Obsidian Volcanic glass are common rhyolitic
flows
11The Grand Canyon of Yellowstone is made out of
rhyolite.
12Basalt flows can also occur at continental hot
spots because some of the magma comes directly
from the mantle.
13Magma Type? Silica? Explosive?
Magma Formation
Lava
Landform
Plate Tectonics
Where on Earth
Rhyolitic
HIGH
Extremely
Increase in temperature
MAINLY Rhyolitic Flows (Obsidian), but also
Basaltic flows.
In Yellowstone this formed a caldera.
Does not occur at a plate boundary.
Yellowstone National Park, Wyoming and Montana