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Magma
Molten rock below ground
Lava
Molten rock once it has reached the surface
Intrusive settings
Cool at depth/underground; loses heat slowly, crystals often grow large
Extrusive settings
Cool at or near the surface; cools rapidly, chill too fast to grow big crystals
decompression, addition of volatiles (water), and heat transfer from rising magma
How does Magma form?
Different rocks melt at different temperatures/pressures depending on their composition. Mafic minerals melt last, while felsic minerals melt first
Why do different rocks melt at different temperatures/pressures?
Aphanitic: fine-grained
Phaneritic: coarse-grained
Porphyritic: has phenocrysts distributed throughout a finer matrix; indicates two stages of cooling
What texture does aphanitic, phaneritic, and porphyritic have?
source rock, partial melting, assimilation, and magma mixing
What factors control magma composition?
Partial melting: when a rock is exposed to higher temperatures the felsic minerals melt first, while mafic minerals melt last
Assimilation: while magma slowly moves upward, it may incorporate the chemistry of surrounding rock that melt due to the heat of the magma
How does magma composition change with partial melting and assimilation?
Geysers
A natural hot spring that intermittently shoots jets of hot water and steam high into the air
They are both created by the same underground plumbing system where there is a circulation of hot, mineral-rich water powered by magma
Why are geysers found near ores?
Gabbro
Is Mafic and can be found in lower oceanic crust
Basalt
Is mafic and can be found in oceanic floor
Granite
Is felsic and is found deep within continental crust
Rhyolite
Is felsic and is found in continental volcanic regions and along convergent plate boundaries
Diorite
Is intermediate and can be found at convergent plate boundaries
Andesite
Is intermediate and can be found at subduction zones and convergent plate boundaries
Volcanic eruptions causes cooling in the short-term because of ash, but causes heating in the long-term because of gases emitted
How can volcanic eruptions affect climate in both the short-term and long-term?
caldera
A large volcanic crater that forms primarily through the collapse of a volcano after a significant eruption, where the ground above an emptied magma chamber sinks inward due to the removal of magma that once supported it
Shield volcano: divergent plate boundaries and hot spots
Cinder cones: flanks of larger volcanoes and in volcanic fields
Stratovolcanoes (composite): convergent plate boundaries where an oceanic plate subducts beneath a continental plate
What are the three main types of volcanoes and where are they found?
Volcanic domes
A steep-sided mound formed by the slow accumulation of viscous lava that cannot flow away easily
Volcanic fissures
A linear volcanic vent through which lava erupts, typically without explosive activity
Volcanic craters
A bowl-shaped depression atop a volcano
its viscosity determines that; the thicker it is the more explosive the volcano
How does magma composition determine the explosivity of a volcano?
Pyroclastic flow
A dense, destructive mass of very hot ash, lava fragments, and gases ejected explosively from a volcano and typically flowing downslope at a great speed
Lahar
A destructive mudflow on the slopes of a volcano
Mt. Vesuvius (Pompeii, Italy)
City buried under 13-20 feet of volcanic ash. Eruption occurred in 79 AD
Mt. Saint Helens
Eruption in 1980 in Washington State. Caused 61 casualties. There was a vertical and lateral blast from the volcano.
Hotspot
An area where hot material from deep within earth’s mantle rises toward the surface, creating volcanic activity
magma is usually basaltic and runny
What is the effect of oceanic crust over a hot spot?
Magma can interact with and melt continental rocks, making it higher in silica and thicker/ more viscous, leading gases to become trapped more easily, causing more explosive eruptions
What is the effect of continental crust over a hot spot?
very explosive magma meaning it has high viscosity and is thick
What magma do you see with a stratovolcano?
Basaltic magma (explosive/runny)
What magma do you see with a cinder cone volcano?
Basaltic magma (gentle/flowing)
What magma do you see with a shield volcano?
earthquake activity
changes in shape
changes in heat flow
increases in gas emission and steam
What are the 4 ways we can predict volcanic eruptions?
freeze/thaw (frost wedging), exfoliation and sheeting, salt wedging, and biological
What are the main types of physical weathering?
dissolution, oxidation, and hyrdolysis
What are the main types of chemical weathering?
They are complementary. Chemical weathering acts on surfaces, which increase due to physical weathering.
How do chemical and physical weathering exacerbate one another?
Soil is the loose material on Earth’s surface that supports plant growth, while sediment mainly consists of rock/mineral particles that can be transported and deposited
What is soil and how is it different from sediment?
The process by which loose sediment is turned into solid sedimentary rock; its two main processes are compaction and cementation
What is lithification and its two main processes?
Siliciclastic (detrital), chemical (biochemical), and organic
What are the main types of sedimentary rock?
conglomerate, breccia, sandstone, siltstone, shale/mudtone
What are the different types of clastic/detrital sedimentary rocks?
As sediment travels farther from its source sorting increases, roundness increases; if its angular and poorly sorted it is usually closer to the source
How do sorting and angularity change with maturity/distance from their source?
tells you the energy of the environment; large grains = high energy, small grains = low energy
What does grain size indicate?
chemical/biochemical, commonly forms from calcium carbonate
What kind of sedimentary rocks are limestone and where/how does it form?
chemical
What kind of sedimentary rocks are evaporites?
biochemical/chemical
What kind of sedimentary rocks are chert?
bedding/layering, cross-bedding, graded bedding, mud cracks, and ripple marks
What are the kind of structures we see in sedimentary rocks?
Metamorphism
Solid-state change due to change in preexisting rock’s environment
heat, pressure, fluids
What are the different types of metamorphic agents/causes?
temperature change, pressure change, compression/shear
What are the different types of metamorphic processes?
Foliated metamorphic rock
Have a layered, or foliated, pattern from the rearrangement or recrystallization of minerals
Nonfoliated metamorphic rocks
Monomineralic rocks with equant grains or not subjected to high enough pressure
slate, phyllite, schist, gneiss
What is the order from low to high grade of these four things? phyllite, schist, gneiss, and slate
shear stress
Causes foliation; crystal grains become elongated, flattened, or aligned in a particular direction
confining stress
Pressure is applied equally in all directions, so crystals tend to become more compact without a preferred alignment (more rounded/compact)
quartzite
What rock forms from the metamorphism of sandstone?
marble
What rock forms from the metamorphism of limestone?
hornfels
What rock forms from the metamorphism of contact metamorphism?
contact (thermal), burial (weight), dynamic (shearing), dynamothermal (regional), hydrothermal, subduction zones, shock
What seven tectonic environments/geological settings do we see metamorphism?
erosion and lithification
How can you change an igneous rock into a sedimentary?
heat and pressure
How can you change sedimentary into metamorphic?