Endogenic Process Flashcards
processes formed or occurring beneath the surface of the Earth
Endogenic Process
mixture of molten rock, minerals and gases
Magma
mixture usually made up of a hot liquid base called the melt,
minerals crystallized by the melt,
solid rocks incorporated into the melt from the surrounding confines and dissolved gases
Magma
the hot liquid base in the magma mixture
Melt
What is the magma made of?
molen rock
minerals
gases
originates in the lower part of the Earth’s crust and in the upper portion of the mantle (asthenosphere)
Magma
Where does the magma originate from?
Asthenosphere
At about __ to __ km below the earth’s surface, the temperature is high enough to melt rocks into magma
30 - 65 km
the temperature rises about __
30ºC/km
How deep is the asthenosphere
100km to 350km
The melt in the magma flows very slowly because it is under __ __
intense pressure
Magma reaches temperatures between __
600ºC to 140ºC
Deep in the Earth,nearly all magmas contain gas dissolved in the liquid, as magma rises at the surface of the Earth, pressure is decreased and the gas forms a __
separate vapor phase
Deep in the Earth,nearly all magmas contain gas dissolved in the liquid, as magma rises at the surface of the Earth, __ and the gas forms a separate vapor phase
pressure is decreased
resistance to flow; antonym for fluidity
Viscocity
Relationship between silica concentration in magma with viscosity
Silica concentration is directly proportionate to viscocity
Magma leaves the confines of the asthenosphere and crust in two major ways
intrusion
extrusion
Magma can be intruded into a __ area of another geologic form. Whe it cools and hardens, this intrusion develops into a __ aka igneous intrusive rock
low-density; pluton
Magma rises towards the Earth’s surface where there are __ dense surrounding rocks and when a __
less; structural zone allows movement
Magma collects in areas called
Magma chamber
Magma develops within the __ and __ where the temperature and pressurre conditions favor the molten state
upper mantle and crust
the __ dense magma __, while the __ dense magma __
less; rises, most; sinks
Ways to Generate Magma
Decompression Melting
Transfer of Heat
Flux Melting
involves the upward movement of the Earth’s mostly solid mantle.
Decompression Melting
The hot material in decompression melting rises to an ara of lower pressure through the process of __
convection
happens when hot liquid rock intrudes the earth’s crust. As the liquid rock solidifies, it loses this heat and transfers it to the surrounding crust (hot fudge and sundae)
Transfer of Heat
when water or CO2 added on rocks affects the melting point of rock when added with water beneath the earth and generates magma
Flux Melting
often generates magma in subduction zones
Flux melting
his magma has high viscosity level, since it has highest silica content.
coolest of all magma types
Felsic Magma
Felsic Magma
Feldspar, Silica
this magma has high viscosity level, low in iron, but high in potassium and sodium
makes granite rocks
Felsic Magma
Felsic magma has:
__ viscosity level
__ iron
__ potassium and sodium
Felsic Magma
This form is normally found in erupting volcanoes, after the eruption, it releases a lava that has high silica and very viscous
commonly produce andesite rock
Intermediate magma
Felsic magma makes __ rocks
Granite
Intermediate magma commonly produces __ rocks
Andesite
has relatively low silica content but high in iron and magnesium
low gas content and viscosity
high average temperature which contributes to its love velocity
most fluid
Mafic Magma
Mafic Magma
Magnesium and Iron
today our planet is too cool for this type of magma to form
hottest and fastest flowing magma
Ultramafic magma
Gabbro and Basalt
Mafic
Diorite and Andesite
Intermediate
Granite and Rhyolite
Felsic
Gabbro, Diorite, Granite
Intrusive Mafic, Intermediate, Felsic respectively
Basalt, Andesite, Rhyolite
Extrusive Mafic, Intermediate, Felsic respectively
Rock Deformation
Stress
Strain
Joints
Faults
force that could create deformation on rocks in their shape and volume
Stress
great forces from several directions may act on lithospheric plates causing them to move. Although, these crustal plates are elastic solid, they are subjected to forces such as pulling, pushing, or squeezing
Stress
2 Kinds of Stress
Lithostatic
Differential
rock beneath earth’s surface experience equal pressure exerted on it from all directions because of the weight of the overlying rock (ex. water pressure on a person’s body)
Lithostatic stress
stress on rocks that are caused by an additional due to unequal stress due to tectonic forces
Differential Stress
3 Types of Differential Stress
Tensional (stretching)
Compressional (squeezing)
Shear (strike-slip)
Stretching
Tensional
Squeezing
Compressional
Strike-slip
Shear
ability of a rock material to handle stress
depends on the elasticity of the rock
Strain
Strain: Faulting - broken block
Brittle deformation
Strain: flow - stretched block
Ductile deformation
fractures in rocks that show little or no movement at all
Joints
long and deep break or large crack in a rock
result of continuous pulling and pushing
Fault
3 Types of Faults
Dip-slip fault (normal fault)
Strike-slip fault
Reverse (or thrust) fault
occurs when brittle rocks are stretched
tectonic tensional forces are involved and the movement of blocks or rocks are mainly in the vertical direction
Dip-Slip faults
Normal fault: the block lying on top of the fault surface is referred to as the __l while the one below is referred to as the __
hanging wall; foot wall
occurs when brittle rocks are sheared and the movement of blocks of rock is chiefly in the horizontal direction
Strike-slip fault
occur when brittle rocks are pushed (compressional)
reverse or thrust fault
believed to impact as the BIG ONE is a dominantly strike-slip fault
West Valley Fault
moves in ann oblique dextral motion
East Valley fault
promoted by high temperature and pressure at a great depth
Folds
when rocks deform in a ductile manner, instead of fracturing to form faults or joints, they may bend or fold and the resulting structures are called __
Folds
3 Types of Folds
Monoclines
Synclines
Anticlines
simplest types of folds.
occur when the horizontal layers are bent upward so that two limbs of the fold are still horizontal
Monocline
fold structures when original rock layers have been folded downward and the two limbs of the fold dip inward towards the hinge of the fold
Syncline
fold structures formed when the originally rock layers have been folded upward and the two limbs of the fold dip away from the hinge of the fold
Anticline