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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. Lava flowing on dry land cools more slowly that lava erupting underwater.
Erosion
Solid-state diffusion
The effect of the environment on eruptive style
Chert
2. 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
B-horizon
Ridge-push force
Diagenesis
Columnar jointing
3. Elongate submarine mountain ranges whose peaks lie only about 2-2.5km below sea level. Consist of a ridge axis - are roughly symmetrical - and can include escarpments - axial troughs - and valleys. Examples - Mid-Atlantic Ridge - East Pacific Rise -
Transition zone
Crust
Mid-ocean ridges
Melting
4. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Crystalline
Strata
Root wedging
5. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Metals
Residual soil
Siltstone and mudstone
Alloy
6. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Deep-ocean trenches
Sedimentary structure
Igneous rocks
Large Igneous Provinces (LIPs)
7. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Calderas
Source rock composition
Area of igneous activity
Basalt
8. Sedimentary rock composed of clay.
The effect of viscosity on eruptive style
Volcanic blocks/bombs
Agrillaceous rocks
Transition zone
9. Distinguishing feature of magma; the process where magma sits in a magma chamber before completely solidifying - it may incorporate chemicals derived from the walls rocks of the chamber.
Laccolith
Assimilation
Mid-ocean ridges
Heat transfer
10. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Transported soil
Polymorphs
Luster
Basaltic lava flows
11. Sedimentary rocks made up of the shells of organisms.
Ultramafic
Melting
Bed
Biochemical sedimentary rocks
12. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Cementation
Five steps of clastic sedimentary rock formation
Bedrock
Intermediate
13. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Seamount chains
Laccolith
Effusive eruptions
Clastic sedimentary rocks
14. 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
Pangaea
Chemical sedimentary rocks
Plate tectonics
15. Soil section below the A-horizon; a soil level that has undergone substantial leaching but has not yet mixed with organic material. Because it lacks organic materials - this horizon tends to be lighter than the A-horizon. Part of the zone of leaching
E-horizon
Partial melting
Ultramafic
Arkose
16. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
a'a'
O-horizon
Gem
Transition zone
17. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Factors of magma cooling time
Color
Reason for Earth's internal heat
Seamount chains
18. Process that occurs after the sediment has been buried - pressure cause by the overburden squeezes out water and air that had been trapped between clasts - and the clasts press together tightly.
The effect of the environment on eruptive style
Zone of leaching
Compaction
pahoehoe
19. An exposure of bedrock.
Outcrop
Facets
Crystalline
Mineral crystal destruction
20. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Basaltic lava flows
Peridotite
ravertine
Volcano
21. Chemical weathering during Which minerals dissolve into water.
Dissolution
Decompression
Deep-ocean trenches
Relative plate velocity
22. By melting - dissolving - or other chemical reactions.
ravertine
Extrusive igneous rock
collision
Mineral crystal destruction
23. Sublayer of the mantle - depth of 660km.
Glassy igneous rocks
The core
Upper mantle
Intermediate
24. 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.
Assimilation
Chemical weathering
Solid-state diffusion
Gem
25. Breaks intact rocks into unconnected grains or chunks - collectively called debris or detritus. Grain size from largest to smallest: boulders - cobbles - pebbles - sand - silt - mud/clay.
Phreatomagmatic eruptions
Sulfides
Jointing
Physical weathering
26. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
Glassy igneous rocks
Arkose
Special properties of minerals
Fissure eruptions/lava plateaus
27. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Melting
Factors classifying clastic sedimentary rocks
Area of igneous activity
Salt wedging
28. A rock made of solid mass of glass - or of tiny crystals surrounded by glass. Reflect light as glass does and tend to break conchoidally. Examples - obsidian - tachylite - pumice.
Solid-state diffusion
Glassy igneous rocks
Continental drift hypothesis
Volcano
29. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Rock composition
Cross beds
Granite
E-horizon
30. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Andesitic lava flows
Relative plate velocity
Redbeds
Weathering
31. Type of volcano; built from ejected lava fragments - cone shaped piles of tephra - steep slope angle - smaller in size - frequently occur in groups - deep craters.
Differential weathering
Cinder cone
Metamorphic foliation
Fractional crystallization
32. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Plates
O-horizon
Lapilli
Volcanic pipes/necks
33. 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.
Batholiths
Reason for Earth's internal heat
Felsic - intermediate - mafic - ultramafic
Pangaea
34. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Slab-pull force
Jointing
Chemical weathering
Tephra
35. Distinguishing feature of magma; the process where different magmas formed in different locations from different sources may come in contact within a magma chamber prior to freezing. Thus the originally distinct magmas mix to create a new - different
Magma mixing
3.5km (2 miles)
Clastic
Paleopole
36. Layering in sedimentary rocks.
Crystal structure
Granite
Bedding
Clastic sedimentary rocks
37. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Alloy
Rock texture
C-horizon
Fumerolic mineralization
38. A mineral's growth that is uninhibited - has well-formed crystal faces.
Thermal expansion
Phreatomagmatic eruptions
Euhedral crystal
Soil Horizons
39. Process where a convergent boundary ceases to exist when a piece of buoyant lithosphere - such as a continent or island arc - moves into the subduction zone. Yield some of the most spectacular mountains/mountain ranges on the planet including the Him
collision
Volatiles
Plutons
Subsidence
40. Sedimentary rocks consisting of carbon-rich relicts of plants.
Organic sedimentary rocks
Lapilli
Spreading rate
Partial melting
41. Cause of melting; when magma rises up from the mantle into the crust - it brings heat with it which raises the temperature of the surrounding crustal rock - and in some cases melting occurs.
Heat transfer
Abyssal plains
Arkose
Igneous rocks
42. The ocean floor is diced up by narrow bands of vertical fractures. Lie roughly at right angles to mid-ocean ridges - effectively segmenting the ridges into small pieces.
Volcano
Solid-state diffusion
Fracture zones
Flood basalts
43. 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
Geothermal gradient
Tephra
Strata
Redbeds
44. The freely pivoting up and down compass needle's angle of tilt relative to the location upon the Earth's surface. At the equator - the specialized magnetic needle would position horizontally and at a magnetic pole it would point straight down.
Ridge-push force
Magnetic inclination
Deep-ocean trenches
Superplumes
45. The transformation of loose sediment into solid rock.
Slab-pull force
Crystal structure
Lava domes
Lithification
46. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Dunes
Solid-state diffusion
Redbeds
Spreading rate
47. 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.
Transgression
Saprolite
Sill
Siltstone and mudstone
48. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Ripples
Regolith
Redbeds
Gem
49. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Mid-ocean ridges
Deep-ocean trenches
Rocks
Convective flow
50. Most common mineral on Earth; compose over 95% of the continental crust. Consist of combinations of a fundamental building block called silicon-oxygen tetrahedron - different groups: independent tetrahedra - single chains - double chains - sheet sili
Dipole
Mid-ocean ridges
Silicate minerals
Stratagraphic formation
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