Geology terms from "Earth's Dynamic Systems" Chapters 1-6
Terms
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- Simple 3 part composition of the earth
- Crust-Mantle-Core
- Lithosphere
- Crust and upper part of mantle
- Asthenosphere
- Less rigid upper part of mantle. Material melts or nearly melts here. Rocks lose strength and become plastic here.
- Mesosphere
- Strong, rigid mantle area. High pressure at this depth offsets the effect of high temperature
- Solid Inner Core
- Dense part of core
- Liquid Outer Core
- Circulation of this part of the core generates Earth's magnetic field. Flows because of heat loss from the core and rotation of the Earth.
- Atmosphere
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-.0001% (2mm over surface)
-all air has water (few % to 100%)
-resting time = 10 days
-it's small, but important, especially storms and distance of water - Hydrosphere
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-Definition: total mass of water of surface of our planet
-Covers about 71% of the surface
-98% in oceans
-Water permitted life to evolve and flourish; every inhabitant on Earth is directly or indirectly controlled by it
-Necessary for life
-Regulates climate
-Transfers heat/mass
-Most important erosion agent on land
-Trap for sediment - Biosphere
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-Definition: the part of the earth where life exists
-Consists of more than 1.6 million described species, 3 million more not yet described
-Uneven, more biomass/species near the equator (warm and wet)
-Fossil fuels from biosphere
-Model for oil/gas environment
-Model for environment of past life
-Model for sedimentary rocks
-Role of life in evolution of crust, atmosphere, hydrosphere
-Main factors controlling the distribution of life on our planet are temperature, pressure, and chemistry of the local environment
-Formed all the Earth’s coal, oil, and natural gas
-Much of the rock in Earth’s crust originated in some way from biological activity - Crust
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-Elevation difference between ocean and continent
-Water runs downhill to basins
-Continental crusts and oceanic crusts - Continental Crust
- Include shields, stable platforms, and folded mountains
- Shields
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-complex of metamorphic rocks and a variety of igneous rocks
-the upper surface is flat and commonly eroded to near sea level
-complexly deformed ancient crystalline rocks exposed at surface
-also called basement rocks, basement complex
-low relief (elevation difference between the low and the high spots), few 100’s of meters elevation, local relief – variability resistant rocks
-complex structure and rock type - Stable Platform
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-no major tectonism
-shield + veneer of sedimentary
-flat lying sedimentary rocks (broad domes, basins)
-craton
-when a basement complex is covered with a veneer of sedimentary rocks - Craton
- the stable continental crust, including the shield and stable platform area
- Basement complex
- rocks of shields are high deformed igneous and metamorphic rocks, covered with a layer of horizontal sedimentary rock
- Folded Mountains
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-rock resistant to erosion, folded, intruded
-along continental margins
-when eroded, form shield, basement
-less dense than ocean
-ancient
-deformed by horizontal stress during slow collision between two lithospheric plates - Oceanic Crust
- Includes oceanic ridge, abyssal floor, seamounts, trenches, and continental margins
- Oceanic Ridge
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-continuous broad fractured rise,
-top of ridge as much as 3000 m higher than adjacent ocean floor
-rift valley - Rift Valley
- crack like surface that runs along the axis of the ridge throughout much of its length, long fracture zones
- Abyssal Floor
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-relatively broad and smooth
-abyssal hills cover much of the sea floor
-abyssal plains - Abyssal Plains
- near continental margins, land derived sediment completely covers abyssal hills
- Seamounts
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-isolated peaks of submarine volcanoes
-some are chains, like Hawaii - Trenches
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-lowest areas on Earth’s surface
-invariably adjacent to chains of volcanoes called island arcs
-linear - Continental Margins
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-continental shelf
-the zone of transition between a continent and an ocean basin
-continental slope-more dense
-young
-not folded like mountain belts - Continental shelf
- submerged part of continent
- Continental Slope
- marks the edge of the continental rock mass, found around the margins of every continent and around smaller fragments, longest and highest slopes on Earth
- Heat Exchange
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-Makes the planet dynamic
-Drives from the interior of the earth
-Convection moves mass - Dynamic
- a system that is composed of individual items or components that work together to make a unified whole, and in this, material and energy move about and change from one form to another
- Conduction
- Heat transfer through a mass
- Convection
- Heat transfer as a result from the movement of a mass
- Radiation
- Heat tranfer from electromagnetic waves from the sun
- Heat Transfer
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-drives hydrologic and tectonic systems
-heat transfers from hotter to cooler regions always - Heat Flow
- Flow of heat from the interior of the earth
- 4 systems of weather and climate
- evaporation, precipitation, condensation, transpiration
- Atmospheric Circulation
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-Hydrologic systems redistribute water across the earth
-Moisture rises with warm air, air cools water falls - Hydrosphere Budget
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-Ocean 97.5% many sources, sinks, evaporation, residence time 3,000 years
-Ice (glacial in Antarctica and Greenland) 2% residence time of 10,000 years
-Groundwater .5% occurs almost everywhere in subsurface, residence time 1 month-100’s of thousands of years, depending usually on how deep it is
-Lakes residence time: 100-200 years
-Rivers residence time: 20 days
-Plants remove a lot of water from the ground
-Streams, ice, waves, groundwater modifies most of surface of continents - Residence time
- average amount of time a tiny bit of water spends in wherever
- Why does the hydrosphere move?
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-Gravity – how does it get to a high location – why not all flowed long since to oceans and stayed there?
-Storms—circulation—heat flow
-Heat source (sun)
-General circular pattern, water vapor redistribution by atmosphere
-currents—driven by wind, upper 300m of ocean - Water vapor redistribution by atmosphere
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-warm, moist air rises at equilibrium, drops rain
-depleted in moisture, cools, drops, warms at 30 degrees
-evaporates water, moves toward poles
-meets cool air at 50 degrees – storms and precipitation - Reservoirs
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Ocean, Ice, Groundwater, Lakes, Atmosphere, Rivers, Living Organisms
*These are driven by convective heat transfer - Ocean
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-97.5% water
-90% returned by precipitation, 10% runoff
-only sink is evaporated
-resting time = 3000 years - Ice
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-80% not in ocean (2% of total)
-nearly all in Antartica and Greenland
-resting time = 10 ka
-melt, sea level change 100m - Groundwater
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-20% not in ocean (.5% total)
-nearly everywhere on land
-soil rest time = 1 month, deep aquifers t=ka to ma - Lakes
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-.7% not in ocean, .02% of total
->half in fresh lakes, mostly in Great Lakes, Baikal, East Africa
-resting time = 100-200 years for large lakes (long time to flush pollution) - Rivers
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-.0001% at any moment
-resting time = maybe 20 days
-small, but important, Transfers water between land and ocean, erosion, transport, etc.
-instantaneous volume is small, but carry large volume over time - Living Organisms
- transpiration – remove perhaps as much water from ground as rivers
- Effects of Hydrosphere
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-enormous energy involved
-modifies and destroys effects of tectonic system
-Finite amount of water
-Can locally change water avail (Las Vegas)
-Irrigation, builds salt, need to flood fields to flush, depletes aquifer, subsidence, etc
-Alter sediment budget, costal erosion, Colorado River - Tectonosphere
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-Helps explain why mountain ranges and mid ocean ridges are located where they are
-Temperature is an important factor - 3 Ways Plates Interact with Each Other
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-Move apart from each other, mainly at mid ocean ridges
-Plates come together
-Plates slide past each other - Theory of Plate Tectonics
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-Movement can be measured (not a theory)
-Mechanisms that drive motion uncertain (being tested theory)
-Plate Tectonics is to geology as DNA is to genetics: unifies, clarifies, explains major features of the earth
-Radical change in the view of the earth - Features of Plates
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-Continental margin + plate margin not always same
-Some plate have no continental material
-Some boundaries uncertain - Convergent Boundaries
- plates come together, produces volcanism, types: oceanic crust to oceanic crust, continental crust to oceanic crust, continental crust to continental crust
- Transform Boundaries
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-Boundary between two moving lithospheric plates, usually along an offset segment of the oceanic ridge
ex: San Andreas Fault - Divergent Boundaries
- plates pulled apart
- Divergent Margins
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-Spreading, upwelling, form of new crust, hot—low p—high, high heat flow (convection)
-Offset by trans. Faults
-New margin – Red Sea vs Atlantic
-Lower top and deeper water at lithosphere cools away from the ridge
-Motion perpendicular to ridge
-Pangaea: super continent that broke up a long time ago
-Lithosphere beings to pull apart
-Rift valley thins
-Crust becomes thin so it produces oceanic lithosphere - Convergent Margins
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-Geology complex and varied
-Cool, hi-p plate descends (subduction) (convection)
-Subduction not necessarily perpendicular to ridge
-Accetionary wedge
-Oceanic-oceanic “island arcâ€
-Ocean-continent(with and without magmatism)(with and without mountain belts)
-continent-continent (not true sub—underring, thickening, compression) - Intraplate Processes
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-Plumes (Hawaii, Yellowstone) (convection)
-Age vs time relation - Tectonic Feature of MOR
- divergent margin
- Tectonic Feature of trench
- convergent margin or sub zone
- Tectonic feature of folded mountain belt or volcanic arc
- convergent margin
- Tectonic feature of volcanism
- margins of all types
- Definition of Mineral
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-Naturally occurring
-Inorganic solid (one exception)
-Internal structure
-chemical composition varies within limits
-exhibits physical properties
-stability limits – but may be broad or narrow
-basic building blocks of rocks - Atom
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-comprised of protons and neutrons, surrounded by electrons, distance across atom is about an angstrom (A with circle over it)
-elements unique by number of protons, and variation in electrons and neutrons
-if e≠Z, it’s an ion (charged)
-the type of bond has a strong influence on mineral property - Covalent Bonds
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-share electrons
-these are strong - Ionic Bonds
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-occurs when one atom in bond gives up an electron/s and the other one takes it, so they become ions with opposite charges, and opposites attract
-these are weak
-tend to come apart in water, soluble in water - Most Common Elements
- H, O, Si, Al, Fe, Mg, Ca, K, Na, C
- Why do Mg and Fe substitute?
- Mg^2+ is .72 ang; Fe^2+ is .78 ang.
- Important properites of structure and composition in minerals
- crystal form, cleavage, hardness, density, color, streak, etc.
- Rock Forming Minerals
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-feld, mica, amph, px, ol, qtz, cc, dol, clay, halite, gypsum
-make up almost all of the upper mantle and crust - Solid Solution
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-can vary within minutes
-Olivine can have formula between MG2SiO4 and Fe2SiO4
-you can’t think of a crystal as a molecule
-for every 19 magnesium atoms, there’s an iron
-narrowly defined limits
-atoms can substitute for each other based on size and charge
-a lot of solid solution substitutes occur for elements on the same column on the periodic table - Physical Structure of Diamond and Graphite
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-Diamond, made out of carbon (covalent bonds really strong)
-Graphite, made out of carbon
-Diamond and Graphite differ in the way the bonds work - Hot Spots
- -melting beneath lithosphere, islands get older and older, Hawaii Island example, Yellowstone
- Plates
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-Plate continental boundaries may be, but need not be, in the same location
-Plate motion differs at boundaries: divergent perpendicular, transform parallel, convergent between - Internal structure of Pyroxene
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-There is a unique manner in which the atoms are bonded together, specific geometric pattern
-Example of a mineral that shows unique internal structure - Which mineral always has a fixed composition?
- Pyrite (FeS2)
- Cleavage
- how a mineral breaks
- Meta Stable
- rock just waiting to be pushed off a cliff, needs the pushing energy to change
- What is the most abundant mineral in the earth's crust?
- Feldspar
- Magma
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-Molten rock [melt+/-gas+/-crystals] cools to igneous rocks
-Hot, partially molten rock material. Most are a combination of liquid, solid and gas.
-Forms igneous rocks when it cools
-Intrusive rock – Magma that solidifies below the surface
-Extrusive rock – Magma that has reached the surface (becoming lava) without completely cooling and flows out over the landscape. - Texture of Magma
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-glassy
-aphanitic
-porphyritic-aphanitic
-porphyritic
-phaneritic
-porphyritic-phaneritic
-pyroclastic - Glassy texture
- Taken from a temperature when crystals would normally form and then cooled rapidly/quenched.)
- Aphanitic texture
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-microscopic crystals [extrusive, cooled quickly, but not too fast, not glassy]
-Relatively rapid cooled
-Made of numerous small spherical or ellipsoidal cavities called vesicles. They are created by gas bubbles trapped in the solidifying rock. - Examples of rocks with Aphanitic texture
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-Rhyolite – Has the same silicic composition as granite. Not common along ocean ridges or oceanic islands but is more common on the continents
-Andesite – Most abundant lava type after basalt. Occurs mostly along convergent plate margins in island arcs and along continental margins. It is rare in oceanic islands.
-Basalt – Most common aphanitic rock. It is abundant on the seafloor
-Komatiite – Rare volcanic rock. Found mostly in very ancient rock sequences exposed in the continental shields. - Porphyritic-aphanitic texture
- aphanitic rock with phenocrysts [like aph, but erupted magma with x’ls]
- Porphyritic texture
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-2 stages of cooling: Initial stage of slow cooling in which large grains develop Followed by a period of more rapid cooling during which the smaller grains formed
-Phenocrysts – larger, well-formed crystals
-Smaller crystals – matrix and the groundmass - Phaneritic texture
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-visible crystals [intrusive, cooled slowly]
-Uniform (very slow) rate of cooling and large crystals
-Composed of grains large enough to be recognized without a microscope - Examples of rocks with phaneritic texture
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-Granite – coarse grained igneous rock composed predominantly of feldspar and quartz
-Diorite – Similar to granite in texture; Plagioclase feldspar is the dominant mineral
-Gabbro – Not usually found at the at the earth’s surface. Makes up the lower part of the oceanic crust and is present at some intrusions. Composed of pyroxene, calcium-rich plagioclase, and olivine.
-Peridotite – Composed mainly of olivine and pyroxene. Makes up a large portion of the mantle and is not common on the surface. - Porphyritic-phaneritic texture
- rock with phenocrysts [intrusive, cooled slowly in two stages]
- Pyroclastic texture
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-ash, crystals, pumice, rock fragments [explosive]
-Produced when explosive eruptions blow crystals and bits of still molten magma into the air as a mixture of hot fragments called ash - Examples of rocks with pyroclastic texture
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-Ash – dust sized pieces
-Pumice – vesicular froth glass common among the lager fragments
-Tephra – shards of volcanic glass, pumice, broken phenocrysts, and foreign rock fragments
-Tuff – the rock resulting from the accumulation of pyroclastic fragments - Extrusive Rock Bodies
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-basalt lava flows
-silicic
-explosive volcanism - Basalt Lava Flows
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-Aa – moves slowly. The hardened crust is broken into a jumbled mass of angular blocks and clinkers.
-Pahoehoe – more fluid than aa flows. “Fossil gas bubbles†make the rock light and porous.
-Vesicles – Small holes formed in a volcanic rock by a gas bubble that became trapped as the lava solidified
-Fissure eruptions – Instead of issuing from a central vent, basaltic lava is commonly extruded from a series of fractures in the crust (fissures).
-Lava lakes – Collapsed caldera (summit craters) that may fill with lava
-Lava tubes – Fluid interior breaks through the crust and flows out.
-Bombs – large projectiles blown from a volcano
-Cinder cone – larger particles that accumulate close to the vent
-Shield volcano – Fluid basaltic lava flows freely for some distance, spreading into a thin sheet or tongue before congealing. Shield volcanoes have wide bases.
-Columnar joints – flows that cool, contract and may develop a system of polygonal cracks. Similar to mud cracks.
-Pillow lava – Extrusion of basaltic lava into water produces a flow composed of a multitude of ellipsoidal masses - Silicic
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-Rhyolite domes
-Stratovolcano or composite volcano – a high, step-sided cone centered around the vent formed by alternating layers of tephra and thick, viscous lava flows or domes
(Lavas, Tephra, Lahar, Calderas) - Explosive Volcanism
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-Like shaking a can of pop – When opened CO2 comes out violently – In a volcano H2O, CO2 and magma come out of solution violently
-Expands and rises in a cloud of ash, pumice, crystals and country rock
-Airfall or flow at hundreds of km/hr at hundreds of degrees Celsius
-Airfall (ash?) – Smaller particles of ash that form ash cloud?
-Welded Tuff – a rock formed from particles of volcanic ash that were hot enough to become fused together
-Lateral blast – blast occurring laterally