Chapter 5 - Volcanoes Flashcards
Where do the majority of magmas originate?
One of three plate-tectonic settings: (1) Divergent plate boundaries (2) over subduction zones and (3) at hot spots.
What is the composition of magma determined by?
By the material(s) from which the melt is derived, and the extent of melting of that source material.
What is a mafic magma/rock?
One that is relatively rich in iron and magnesium.
What are felsic rocks/magma?
Relatively silica-rich magmas are usually rich in aluminum as well, so they make rocks rich in feldspar and quartz.
What are the two ways melting can occur?
Reduction in pressure and the addition of fluids (such as water).
What are the two ways a magma’s composition change?
Through fractional crystallization - cools for a short period in magma chamber and some minerals crystallize- and interaction with crust material.
What does the partial melting of the mantle account for?
Basalts (mafic volcanic rock) that form new sea floor at spreading ridges.
How does mafic magma change comp. while traveling through a continental rift zone?
It can be basaltic, silica-rich rhyolite or andesite (intermediate comp.)
What is known as a fissure eruption?
The eruption of magma out of a crack in the lithosphere, rather than from a single pipe or vent.
What is known as the ring of fire?
The collection of volcanoes rimming the Pacific Ocean, which is actually a ring of subduction zones.
What is a shield volcano?
Very flat and low in relation to its diameter, and large in areal extent, usually mafic basaltic volcanoes
What is a cinder cone?
When cinders fall close to the vent from which they are thrown can pile up into a very symmetrical cone-shaped heap.
What are pyroclastics?
Energetically erupted bits of volcanic material.
What are stratovolcanoes?
They are volcanoes built in a layer-cake fashion and are made of more than one kind of material.
What is a lava dome?
When slow-flowing rhyolithic and andesitic lavas ooze out at the surface, piling up close to the volcanic vent, which results in a compact and steep-sided structure.