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Geology
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Subject
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science
Instructions:
Answer 50 questions in 15 minutes.
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Match each statement with the correct term.
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This is a study tool. The 3 wrong answers for each question are randomly chosen from answers to other questions. So, you might find at times the answers obvious, but you will see it re-enforces your understanding as you take the test each time.
1. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Spreading rate
Residual soil
Granitic composition
Biochemical sedimentary rocks
2. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Paleopole
Upper mantle
Carbonate rocks
Chert
3. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Partial melting
Basalt
Volatiles
Siltstone and mudstone
4. Two different minerals which have the same composition but have different crystal structures.
Granitic composition
Saprolite
Magnetic reversals
Polymorphs
5. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Specific gravity
Salt wedging
Sedimentary structure
Felsic - intermediate - mafic - ultramafic
6. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Dike
Transgression
Hardness
Paleopole
7. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Root wedging
Effusive eruptions
Geothermal gradient
Seamount chains
8. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Regression
Limestone
pahoehoe
Sedimentary Basins
9. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Native metals
Mineral
Turbidite
Superplumes
10. Forms when clots of lava fly into the air in lava fountains and then freeze to form solid chunks before hitting the ground. Some forms when the explosion of a volcano shatters preexisting rock and ejects the fragments over the countryside.
Marine magnetic anomaly
Pyroclastic debris
Magnetic reversals
Volatiles
11. Rocks that forms by the freezing of lava above ground - after it spills out (extrudes) onto the surface of the Earth and comes into contact with the atmosphere or ocean.
Chemical weathering
Turbidite
Extrusive igneous rock
Fractional crystallization
12. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Chemical sedimentary rocks
Tuff
Thermal expansion
Sulfides
13. Mineral class; the fundamental component within these types of minerals in the Earth's crust is the silicon-oxygen tetrahedron anionic group - a silicon atom surrounded by four oxygen atoms that are arranged to define the corners of a tetrahedron - a
Melting
Silicates
Andesitic lava flows
Area of igneous activity
14. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Oxides
Organic chemicals
Biomineralization
Depositional environment
15. A mineral's growth that is uninhibited - has well-formed crystal faces.
Evaporites
Euhedral crystal
Pyroclastic flows
Special properties of minerals
16. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Sedimentary rocks
A-horizon
Intermediate
Earth's atmosphere
17. Core division; from a depth of 5155km down to Earth's center at 6371km. A radius of about 1220km - is solid iron-nickel alloy - can reach temperature of 4700 degrees C. Solid in nature because of subjection to greater pressure - keeps atoms from wand
Fissure eruptions/lava plateaus
Color
Laccolith
Inner core
18. Type of volcanic eruption; takes place when water gains access to the hot rock around the magma chamber and suddenly transforms into steam - a pyroclastic eruption involving the reaction of water with magma.
Ridge-push force
Phreatomagmatic eruptions
C-horizon
Soil erosion
19. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Why magma rises
Abyssal plains
Shield volcano
Differential weathering
20. Sedimentary rocks made up of the shells of organisms.
Deposition
Spreading rate
Biochemical sedimentary rocks
Crystalline igneous rocks
21. Consists of rock and sediment that has been modified by physical and chemical interaction with organic material and rainwater - over time - to produce a substrate that can support the growth of plants.
3.5km (2 miles)
Soil
O-horizon
The effect of viscosity on eruptive style
22. The base of the soil profile; consists of material derived from the substrate that's been chemically weathered and broken apart - but has not yet undergone leaching or accumulation.
C-horizon
Felsic - intermediate - mafic - ultramafic
Lava domes
Soil Horizons
23. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Sedimentary structure
Lower mantle
Intrusive igneous rock
Outcrop
24. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
Tuff
pahoehoe
Depositional environment
Volcanic pipes/necks
25. Mineral class; consist of a metal cation bonded to the anionic group. Many form by precipitation out of water at or near the Earth's surface. Example - gypsum.
Magnetic inclination
Sulfates
Ridge-push force
Igneous rocks
26. Mineral class; consist of a metal cation bonded to a sulfide anion. Examples - galena and pyrite. Many have a metallic luster. Can also be considered ores with high proportions of metal within the mineral.
Sulfides
Light silicates
Sandstone
Paleomagnetism
27. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Convective flow
Facets
Batholiths
Siltstone and mudstone
28. The way in which the atoms are packed together within a mineral by chemical bonds. Five difference types of bonding can occur - covalent - ionic - metallic - Van der Waal's - and hydrogen.
Light silicates
Upper mantle
Crystal structure
Symmetry
29. Type of soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
B-horizon
Cementation
Biomineralization
Laterite
30. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Factors classifying clastic sedimentary rocks
Partial melting
Silicate minerals
31. Sea-floor spreading proponents - Hess and others realized that in order for the circumference of the Earth to remain constant through time - ocean floor must eventually sink back into the mantle. This sinking process consumes the ocean floor between
Sea-floor spreading
Subduction
Carbonates
Crystalline igneous rocks
32. Places where intrusive igneous rock creates tabular intrusions cutting across rock that does not have layering - this nearly vertical - wall-like tabular intrusions is formed. Cut across layering within the earth.
Dike
Lapilli
Redbeds
Tuff
33. Refers to the proportions of different chemicals making up the rock - and thus the proportion chemicals affects the proportions of different minerals constituting the rock.
Rock composition
Organic chemicals
Laterite
Lava
34. The angle between the direction that a compass needle points at a given location and the direction of the 'true' (geographic) north. Through this process - the magnetic poles never stray more than 15 degrees of latitude from the geographic pole.
Magnetic declination
Ripples
Partial melting
Cement
35. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Transform fault
Earth's atmosphere
Source rock composition
Melting
36. A fine spray of lava instantly freezes to form fine particles of glass.
Felsic
Soil erosion
Ash
Volcanic blocks/bombs
37. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Granitic composition
Slab-pull force
Alloy
Superplumes
38. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Mafic
Conglomerate
Lava
Rocks
39. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Intermediate
Light silicates
Agrillaceous rocks
Marine magnetic anomaly
40. In degrees Celsius - the high temperatures at which igneous rocks freeze; the freezing of liquid melt to form solid igneous rock represents the same phenomenon as the freezing of water - except at much higher temperatures.
Evaporites
650-1100 degrees C
Solid-state diffusion
Clastic
41. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Polymorphs
Chemical sedimentary rocks
Clastic
Euhedral crystal
42. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Phreatomagmatic eruptions
Color
Hydrolysis
Sulfates
43. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Metamorphic foliation
Outcrop
Graded bed
Sea-floor spreading
44. The removal of soil by running water or by wind.
Mafic
Soil erosion
Crystal
Chemical weathering
45. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Hydrosphere
Clastic sedimentary rocks
Felsic
Arkose
46. Core division; between 2900 and 5155km deep. Liquid iron alloy - it exists as a liquid because the temperature here is so high that even the great pressures squeezing the region cannot lock atoms into a solid framework. This liquid iron alloy is able
A-horizon
Outer core
The core
Why magma rises
47. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Facets
Tephra
Peridotite
Volcanic pipes/necks
48. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Siliceous rocks
Continental shelf
Symmetry
Plate tectonics
49. A plate boundary at which two plates move apart from one another by process of sea-floor spreading. Mid-ocean ridges or simply a ridge. New crust is formed at ridges through the buoyant rising of magma from beneath the surface and solidifies to creat
Basalt
Chert
Mantle
Divergent plate boundary
50. Mineral crystal formation type; form by type of diffusion - the movement of atoms or ions through a solid to arrange into a new crystal structure; process takes place very slowly.
Metamorphic foliation
Polymorphs
Solid-state diffusion
Light silicates
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