Magma Flashcards
Where does lava come from?
The mantle
The lithosphere does not float on a layer of magma, the asthenosphere (mantle) consists of:
solid rock that can flow
The mantle melts when:
- Pressure on the rock is reduced (decompression melting)
- Water (or another volatile) is added to the rock
- Hot, rising magma comes in contact with other rocks and then melts them
When rock rises from point A to point B: pressure decreases a lot, but:
only cools a little, so it melts
What is assimilation?
A block of rock falls into magma and melts
What is contamination?
partial melting of rock mixes with magma from below
Where does magma come from?
- Convergent boundary (seawater stored in the crust is released, water released from hydrous minerals is heated up, melting of the overlying mantle due to addition of volatiles)
- Divergent boundary (hot rocks rise, pressure drops, decompression melting)
- Hotspots
Magma is classified into four groups based on how much silica (silicon and oxygen) is in the magma
- Felsic (most silica)
- Intermediate
- Mafic
- Ultramafic (least silica)
What factors control magma composition?
- Composition of source rock (rock that melted)
- Partial melting (preferentially melts more silica-rich minerals b/c lower melting temp)
- Crystal settling (mafic minerals form first and settle out of melt forming a cumulate, residual rock is richer in silica (more felsic), extracts mafic minerals, increasing silica content in the magma)
- Magma mixing
- Assimilation and contamination
What is a discontinuous reaction?
When minerals become unstable with changing temp. They break down to form new minerals.
What is a continuous reaction?
When the composition of plagioclase changes with changing temp
Felsic minerals melt and crystallize at
low temperatures
Mafic minerals melt and crystallize at
high temperatures
How fast does molten rock cool into igneous rock?
Depends on:
- Depth of the magma: magma deep in the Earth will cool more slowly than shallow magma, and shallow magma will cool more slowly than lava
- Size and shape of magma body: The more S.A a body of magma (an intrusion) has, the faster it will lose heat. Rate of S.A to vol increases and size decreases. (basically the smaller it is, the faster it cools)
- The presence of groundwater: Water passing through magma absorbs and carries away heat, can also create geysers.