Geology 101
Plate tectonics
The study of the origin and evolution of the Universe is called ............. cosmology
The theory that describes the formation of the universe is called ........big bang. According to this theory, the universe evolved ..........13.8. billion years ago from a very high density and high temperature state and keeps ...........expanding.. since that time.
The Solar System (and the Earth) formed about ........4.6.....billion years ago
The process of formation of Earth’s layers is called .......differentiation....... The denser layer (composed of primarily Fe and some Ni) is in the middle and it is called .........the core....; it has two parts – solid ........inner..... and liquid ........outer.....
The presence of liquid metallic elements in the outer core of rotating Earth creates the Earth’s .......magnetic field......
The magnetic field is not static, the magnetic poles switch periodically in the process called magnetic ......reversals........
The Earth middle layer is called .......mantal....... It is also composed of several layers: the
outermost one is rigid, while the one below - .......asthenosphere...... - is plastic (partially molten), while the rest of the mantle is solid
The Earth’s crust can be of two types: ......continental....... and .......oceanic......
Continental crust is .......less...... dense than oceanic
Continental crust is .......more...... thick than oceanic.
The Earth has several different “spheres”: .......lithosphere......sphere –the outermost rigid layer composed of the crust and upper rigid mantle, .....hydrosphere........sphere (ocean, surface and ground waters), ......atmosphere.......sphere (air) composed of mainly ......nitrogen....... and .........oxygen.....
.......Alfred Wegener......is believed to be a father of the theory called plate tectonics
According to this theory, the lithospheric plates are not static, they move around colliding
with each other
The evidence of .......continental drift...... include:
Matched fit of continents
Climate belts
Fossil distributions
Rock unit distributions
Radiating glacial patterns
Paleomagnetic studies
GEOL101, Spring2025
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The evidence of ........seafloor spreading.... include:
Stripped pattern of magnetic field (magnetic reversals)
Seafloor ridges and transform faults
A lithospheric plate consists of ......crust....... and ......upper mantel.......
There are about ......12....... plates, and they move at the velocity of 1 -15 ............./yr
Plate tectonics are driven by ........convection currents..... in asthenosphere
At .....divergent........-plate boundaries, plates pull apart and ......rifiting or spreading....... occurs.
......convergent.......-plate boundaries result in mountain building.
At .....transform........-plate boundaries, plates slide past one another.
There were a few supercontinents in the Earth’s history. The latest one was called .......Pangea......, and it started to break apart around .......200...... Million years ago.
Minerals
Mineral is a naturally occurring, inorganic solid with a specific internal structure. It has a chemical composition that varies within certain limits and can be expressed by a chemical formula.
Minerals are “.....building blocks........” of rocks
There are about .......4,000...... known minerals
To be called a mineral, the substance should have .......5......(how many) characteristics:
Solid of Liquid? solid
Organic or inorganic? inorganic
Artificially made of naturally occurring? Natural occurring
Defined internal structure or chaotically organized one? Defined structure
Defined chemical formula or does not matter? Defined chemical formula
Minerals are grouped based on their chemical formula
The majority of mineral are .......silicates...... (SiO2)
Another large class is .......carbonates...... (CaCO3)
Minerals are identified based on their ......anions.......
.......color...... is not a good characteristic for some minerals, for example ........quartz..... (SiO2), which can be of many colors, while is very good for others (sulfur is .......yellow......, malachite is ......green.......)
The color of the powder that mineral leaves behind is called ......streak........
.......luster...... is the way that light interacts with the surface of a mineral. It can be .......metallic...... and ........nonmetallic.....
.......hardness...... is measured by the resistance to abrasion. The hardness of .....glass........ is 5.5
.......specific gravity.... - the weight of the mineral over weight of equal water volume
Crystal habit and crystal form – the way the crystal ......grows.......
Fracture vs cleavage – the way the mineral .....breaks........
Rocks are ........assemblages..... of minerals
Rocks are .......coherent...... (i.e. forming a whole), naturally occurring solid, consisting of an .........assemblage... of minerals, or, less commonly, of ........glass......
The rock can be ......glassy.......– composed of glass (example: .......obsidian......), or non-glassy – either ......crystalline....... (made up of crystals welded together) or .....clastic....... (composed of individual grains)
Rocks and Rock cycle
There are .....3........ major types of rocks:
.....sedimentary........ – are formed from clasts (or .....grains........) of pre-existing rocks and are held together by .......cement......, or formed by mineral ......precipitation....... the solution (such as rock salt)
........igneous.....– are formed by solidification from molten state. They are composed of .......crystals or minerals...... interlocked together (example: granite, basalt), or rarely, of ........glass..... (example: obsidian)
.......metamorphic......– are formed in a very high heat and pressure, resulting in a ......transformation....... of a pre-existing rock (examples: marble, slate, gneiss, schist).
The ........texture..... of a rock is the size, shape, and arrangement of the grains (for .....sedimentary........
rocks) or crystals (for ......igneous....... and .....metamorphic........ rocks).
.......thin section...... is a very thin slice of rock allowing to study details of the rock texture
........rock cycle**..... is an idealized cycle of processes undergone by rocks in the earth's crust
......rock cycle....... involves igneous intrusion, uplift, erosion, transportation, deposition as
sedimentary rock, metamorphism, remelting, and further igneous intrusion.
GEOL101, Spring2025
Igneous Rocks
Molten rock on Earth’s surface is called ........lava....., beneath Earth’s surface - .......magma.......
Melting of solid rocks occurs as a response to changing .......temp......and .........pressure.....
........decompression..... melting occurs at mid-ocean ridges and rifts. .....flux........ melting occurs above subducting plates.
Melt composition is controlled by .....partial........ melting (......felsic...... melts first) and ........assimilation..... (blocks of rocks fall into magma and melt). ......xenoliths...... are chunks of wall rock incorporated into the magma.
.......mafic...... minerals (rich in Fe and Mg) are first to crystallize and ......last....... to melt.
.......felsic..... minerals (rich in Si, Al, K) crystallize ......last....... and are first to melt.
Magma rises because it is ......buoyant....... and because of pressure from overlying rocks.
Movement rates are directly controlled by a magma’s .....viscosity......... Felsic magma is .......more...... viscous than mafic one.
If magma solidifies within the rock, ......sills.... (horizontal), ........dikes..... (vertical), ........plutons..... (blob-shaped) and .......laccoliths...... (mushroom-shaped) structures are formed.
The rate of .....cooling rate........ depends on the size, depth and composition of an intrusion.
Igneous rocks are categorized based on their .......texture...... and .......composition.......
Composition is dependent on the .....source......... Texture is dependent on ......??........
.........extruded.... rock cools rapidly, and crystals do not have time to grow large. .....intrused........ rock
cools slowly and have large crystals.
......porfirated?....... texture: both small and large crystals (called .......themophist?......), indicating a initial
.......slow...... cooling followed by ......rapid.......cooling (usually after an eruption)
Sedimentary Rocks and Soil
Geologists define .......4...... (how many) sedimentary rock classes:
.......clastic......: loose rock fragments (clasts) cemented together
.......biochemcal......: cemented shells of organisms
........organic.....: carbon-rich remains of once-living organisms
.......chemical......: minerals that crystallize directly from water
Processes that break up rock into sediments is called .......weathering......; removal of grains is called .........erosion..... Major erosional agents are: .......water......, ......ice....... and .......wind.......
Weathering may be of .........3.... (how many) types: ......physical......., .......chemical...... and ......biological.......
Clastic sedimentary rocks are formed when weathering and erosion create ......sediments......., that are later transported, deposited and .....lithification........ (cemented).
Clastic sedimentary rocks are classified based on their ......texture....... (grain size, angularity and sphericity. sorting) and ......composition....... (clast composition, character of cement).
Biochemical sedimentary rocks are made of sediments derived from the shells of once-living organisms (fossiliferous limestone (mineral .............) and chert (mineral .............)). Page 4 of 5
GEOL101, Spring2025
Chemical sedimentary rocks are composed of minerals ......precipitation....... from water solution (.........limestone.... – CaCO3 precipitated from ground water) or ....evaporated......... from seawater (NaCl - .....halite........)
Organic sedimentary rocks are made of organic carbon, the soft tissues of living things
(.......coal...... - altered remains of fossil vegetation and ........oil.....- shale with heat-altered
organic matter).
......breccia....... is clastic sedimentary rock with angular fragments of rock in finer-grained matrix. The one with rounded pebbles of rock is called ......conglomerate........
.......arkose......—sand and gravel with abundant feldspar.
....sandstone.........—clastic rock made of sand-sized particles.
Silt-sized sediments are lithified to form ........siltstone...... Clay-sized particles form mudstone or .......shale.......
....sedimentary structures.........are features that form when sediments are deposited. They include bedding, ripple marks and dunes, cross-bedding, graded beds, mudcracks, etc.
Sedimentary structures tell us about the ......paleoenvironment......., such as glacial, desert, coastal, fluvial environments.
Sedimentary ......basins....... are special places that accumulate sediment. They may be ........foreland..... (in front of mountains), .....intracontinental........ (far away of tectonic boundaries), ....passive-margin......... basins (created as a result of continental rifting) and .............basins (formed at the edges of continents that are not tectonic-plate boundaries).
A sea-level fall or ....regression......... shifts environments toward the basin. A sea-level rise or ......transgression....... shifts depositional bets landward.