| Term | Definition |
|
lava flows |
Rivers of red hot lava. |
|
magma |
Hot liquid that is created deep underground beneath the earth's crust. |
|
vents |
Holes where magma comes to the earth's surface. |
|
pyroclastic material |
Magma and pieces of rock that fly through the air in a wreck of destruction during a violent eplosive eruption. |
|
volcano |
A build-up of pyroclastic material or magma on earth's surface. |
|
water |
This thirst-quinching natural liquid causes eruptions to be more explosive. |
|
silica |
This mineral block causes eruptions to be more violent the more it has of it. |
|
volcanic blocks |
Large pieces of pyroclastic material that is made up of rock. |
|
blocky lava |
a cool stiff lava that can't move very far from the vent. |
|
pahoehoe |
A type of lava that is slow-moving, and is like wax. It resembles rope. |
|
Aa |
A brittle stiff lava. |
|
volcanic bombs |
Blobs of magma that harden in the air. |
|
lava |
magma that has been exposed to oxygen. |
|
pillow lava |
Lava that forms during underwater eruptions. |
|
lapilli |
Pebble sized bits of pyroclastic material that vary between 2 and 64mm in diameter. |
|
volcanic ash |
Forms when stiff magma quickly expands. Is less than 2mm in diameter. |
|
shield volcanoes |
Built out of layers on runny, non-explosive lava. They are large and non-explosive. |
|
cinder cone volcano |
A volcanic cone created entirely from pyroclastic material. They are small and explosive. |
|
composite volcanoes |
They are built out of pyroclastic material and layers of runny non-explosive lava. Are sometimes explosive, and sometimes aren't. |
|
stratovolcano |
Another name for composite volcano. |
|
crater |
A funnel shaped pit and the main vent or a volcano. |
|
caldera |
Forms when a magma chamber empties, and the ground above it falls in, creating a large, sinking depression. |
|
fissures |
Large cracks in the earth's crust. |
|
lava plateaus |
They form similarly to sheild volcanoes; built out of layers of runny, non-explosive lava. They aren't volcanoes. |
|
Mauna Kea |
An example of a shield volcano. |
|
Paricutin |
An example of a cinder cone volcano. |
|
Mount Fuji |
An example of a composite volcano. |
|
extinct volcano |
A volcano that hasn't erupted in recorded history and most likely will never erupt again. |
|
dormant volcano |
A volcano that doesn't show signs of erupting but has erupted in recorded history. |
|
active volcano |
A volcano that shows signs of erupting. |
|
seismograph |
An instrument that measures earthquakes. If many earthquakes that are small occur in a reletively short amount of time around a volcano, it may mean that the volcano is going to erupt soon. |
|
tiltmeter |
An intrument that measures the difference of the sope of a volcano that can change, leading scientists to believe whether or not it will erupt. It isn't 100% accurate. |
|
rift |
A deep crack. |
|
hot spots |
When tecontic plates meet directly below a mantle plume, it forms these. |
|
mantle plumes |
columns of rising magma. |
|
false |
TRUE OR FALSE: A rift and a fissure are the same thing. |
|
false |
TRUE OR FALSE: A caldera is smaller than a crater. |
|
false |
TRUE OR FALSE: A caldera and a crater are formed similarly. |
|
true |
TRUE OR FALSE: A caldera is much larger than a crater. |
|
true |
TRUE OR FALSE: Aa is a stiff, brittle lava. |
|
true |
TRUE OR FALSE: The more silica, the larger the eruption. |
|
false |
TRUE OR FALSE: The less water, the larger the explosion. |
|
false |
TRUE OR FALSE: A stratovolcano is another name for shield volcano. |
|
true |
TRUE OR FALSE: A stratovolcano is another name for a composite volcano. |
|
true |
TRUE OR FALSE: A stratovolcano is not a cinder cone volcano. |
|
false |
TRUE OR FALSE: Cinder cone volcanoes are most often the biggest type of volcano. |
|
cinder cone volcano |
CHARACTERISTICS: A small, explosive volcano that is made entirely from pyroclastic material. |
|
shield volcano |
CHARACTERISTICS: A gigantic, non explosive volcano made from repeated layers of non-explosive lava. |
|
composite volcano |
CHARACTERISTICS: A combination completely of the other 2 types of volcanoes, forms by both repeated layers of runny lava and by pyroclastic material, its' size can vary, and can be both explosive and non-explosive. |
|
divergent boundary |
GOOD TO KNOW: This boundary almost always forms a non-explosive volcano. |
|
convergent boundary |
GOOD TO KNOW: This boundary usually forms explosive volcanoes. |