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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 soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
Quartz sandstone
Turbidity current
Laterite
Bed
2. Sublayer of the mantle - depth of 660km.
Upper mantle
3.5km (2 miles)
Cinder cone
Basaltic composition
3. 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
Streak
Symmetry
Inner core
The effect of gas pressure on eruptive style
4. Forms a 2885-km-thick layer surrounding the core. In terms of volume - it is the largest part of the Earth. It consists entirely of ultramafic rock - peridotite.
Euhedral crystal
Flood basalts
Topography
Mantle
5. Rocks with a fragmental texture consist of igneous fragments that are packed together - welded together - or cemented together after having solidified. Examples - pyroclastic rocks such as tuff or breccia.
collision
Fragmental igneous rocks
Ridge-push force
Continental rift
6. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Alloy
Transition zone
Evaporites
7. Heat from an intense surface fire bakes and expands the outer layer of the rock. On cooling - the layer contracts - causing the outer part of the rock spall - or break off in sheet-like pieces.
Ripples
Laccolith
Thermal expansion
Factors of magma cooling time
8. Chemical weathering during Which minerals dissolve into water.
Dissolution
Magma mixing
Turbidite
Soil erosion
9. Natural cracks that form in rocks due to removal of overburden or due to cooling.
C-horizon
Jointing
collision
Continental shelf
10. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Caliche
Melting
Rock layering
Phreatomagmatic eruptions
11. Outer surface level of Earth; composed of granite - basalt - and gabbro. Continental: mostly about 35-40km thick . Oceanic: about 7-10km thick. Oxygen - by far the most abundant element.
Composite cone (stratovolcano)
Organic sedimentary rocks
Oxidation
Crust
12. 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.
Large Igneous Provinces (LIPs)
Phreatomagmatic eruptions
Igneous rocks
Turbidity current
13. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Volatiles
a'a'
Fracture and cleavage
Laccolith
14. Mineral group; feldspars - quartz - muscovite - clay minerals.
Subsidence
Light silicates
Geothermal gradient
Shield volcano
15. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Conglomerate
triple junction
Lithosphere
12km
16. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
rifting
B-horizon
Earth's atmosphere
Subduction
17. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Facets
The effect of viscosity on eruptive style
Euhedral crystal
Elemental composition of Earth
18. Mineral crystal formation type; from directly from a vapor - occurs around volcanic vents or around geysers. At such locations - volcanic gases or steam enter the atmosphere and cool - so certain elements cannot remain in gaseous form.
Fumerolic mineralization
Volatiles
Evaporites
Inner core
19. Physical property of a mineral; refers to the shape (morphology) of a single crystal with well-formed crystal faces - or to the character of an aggregate of many well-formed crystals that grew together as a group. Depends on the internal arrangement
Crystal habit
Saprolite
Ultramafic
Transgression
20. Process occurring in arid climates - dissolved salt in groundwater precipitates and grows as crystals in open pore spaces in rocks. This process pushes apart the surrounding grains and so weakens the rock that when exposed to wind or rain - the rock
Salt wedging
Transform plate boundary
rifting
Slab-pull force
21. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Frost wedging
Sandstone
Ripples
Shield volcano
22. An exposure of bedrock.
Decompression
Pyroclastic flows
Chert
Outcrop
23. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Reason for Earth's internal heat
Halides
Batholiths
ravertine
24. 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
Xenolith
Partial melting
Silicates
Continental shelf
25. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Root wedging
Xenolith
Streak
Composite cone (stratovolcano)
26. An insulated - tunnel-like conduit through which lava moves within a flow.
Lava tube
Agrillaceous rocks
Fissure eruptions/lava plateaus
Luster
27. The most common minerals in the Earth. Contain silica (SiO2) mixed in varying proportions with other elements (typically iron - magnesium - aluminum - calcium - potassium - and sodium).
Deposition
Silicate minerals
Peridotite
Regolith
28. After sand has lost its feldspar composition due to weathering over time - sediment composed entirely of quartz grains gets buried and lithified to form this type of rock.
Glass
Lava tube
Magma mixing
Quartz sandstone
29. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Turbidity current
Basaltic magma
Seamount chains
Transgression
30. The transformation of loose sediment into solid rock.
Lithification
Decompression
Basalt
Columnar jointing
31. When silt and clay accumulate in the flat areas bordering a stream - lagoon - or delta - the silt when lithified becomes this type of sediment. And the mud - when lithified - becomes another type of sediment - also known as shale.
Sea-floor spreading
Fracture zones
Tephra
Siltstone and mudstone
32. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Transform plate boundary
Relative plate velocity
Effusive eruptions
Biomineralization
33. Distinguishing feature of magma; the process where magma changes composition as it cools because formation and sinking of crystals preferentially remove certain atoms from the magma.
Fractional crystallization
Rocks
Compaction
Residual soil
34. Physical property of a mineral; represents the density of a mineral - as specified by the ratio between the weight of a volume of the mineral and the weight of an equal volume of water a 4 degrees C.
Specific gravity
Continental rift
Sulfides
Why magma rises
35. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Reason for Earth's internal heat
Magnetic anomaly
Calderas
Magma mixing
36. The four classes of igneous silicate rocks based on the proportion of silicon to iron and magnesium. As the proportion of silicon in a rock increases - the density decreases - thus felsic rocks are less dense than mafic. In order - from greatest to l
Outer core
Felsic - intermediate - mafic - ultramafic
Composite cone (stratovolcano)
Rock composition
37. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Hydrolysis
Fractional crystallization
Chemical weathering
Sedimentary rocks
38. 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.
Crystal structure
Chemical weathering
Plate tectonics
rifting
39. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Fractional crystallization
Crystalline
Ultramafic
Crystal lattice
40. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Regolith
Felsic - intermediate - mafic - ultramafic
Metals
Glassy igneous rocks
41. Low-viscosity (basaltic) lava flows out of a volcano easily - whereas high-viscosity (andesitic and rhyolitic) lava can clog and build pressure within a volcano. Basaltic eruptions are typically effusive and produce shield volcanoes - whereas rhyolit
Source rock composition
Xenolith
The effect of viscosity on eruptive style
Siltstone and mudstone
42. The rate of increase in temperature - decreases with increasing depth. The dashed lines represent the solidus and liquidus for mantle rock (peridotite). The solidus line defines the conditions of pressure and temperature at Which mantle rock begins t
Native metals
Geothermal gradient
Upper mantle
Zone of accumulation
43. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
Transition zone
Ultramafic
Biomineralization
Decompression
44. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Hot spots
Metals
Dolostone
Mantle
45. The intrusion of numerous plutons in a region - produces a vast composite body that may be several hundred kilometers long and over 100km wide; an immense body of igneous rock.
Thermal expansion
Elemental composition of Earth
Batholiths
Transform fault
46. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Luster
Lava domes
Stratagraphic formation
Volatiles
47. Develops because mid-ocean ridges lie at a higher elevation than the adjacent abyssal plains of the ocean. The surface of the sea floor overall slopes away from the ridge axis. Gravity causes the elevated lithosphere at the ridge axis to push on the
Paleopole
Ridge-push force
Cementation
Apparent polar-wander path
48. Center of the Earth - consists mainly of iron alloy.
Laterite
Coal
Chert
The core
49. Distinct internal laminations within a ripple or dune that are inclined at an angle to the boundary of the main sedimentary layer. Form as a consequence of the evolution of dunes or ripples.
Cross beds
Organic chemicals
Apparent polar-wander path
Phreatomagmatic eruptions
50. The most important mineral group; comprise the most rock-forming minerals - they are very abundant due to large % of silicon and oxygen in Earth's crust. Examples - oxygen - silica - aluminum.
Pangaea
Rock-forming silicate minerals
Reason for Earth's internal heat
C-horizon
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