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Test your basic knowledge |
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. Alfred Wegener's suggestion that the positions of the continents change through time as they drift away from each other. The flaw was that he lacked a plausible moving mechanism.
Subduction
Fracture zones
Hydrolysis
Continental drift hypothesis
2. Sedimentary rock composed of calcite or dolomite.
Carbonate rocks
Lithification
Fractional crystallization
Salt wedging
3. Places with particularly voluminous quantities of magma erupting or intruding.
Differential weathering
Large Igneous Provinces (LIPs)
C-horizon
Soil
4. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Large Igneous Provinces (LIPs)
Granitic composition
Deep-ocean trenches
Composite cone (stratovolcano)
5. Type of volcano; most are adjacent to the Pacific - larger in size - interbedded lavas and pyroclastics - consist of alternating layers of lava and tephra - most violent type of activity - may produce nuee ardente or lahars.
Composite cone (stratovolcano)
Fumerolic mineralization
Siliceous rocks
Cement
6. 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
Precipitation
collision
Chemical weathering
Soil Horizons
7. 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.
Ripples
Heat transfer
Marine magnetic anomaly
Hot-spot track
8. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
3.5km (2 miles)
Conchoidal fractures
Quartz sandstone
Root wedging
9. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Carbonate rocks
Continental drift evidence
Why magma rises
Sandstone
10. Some rock bodies appear to contain distinct formations - defined either by bands of different compositions or textures - or by the alignment of inequant grains so that they trend parallel to one another.
atmospheres (atm)
Diagenesis
Mafic
Rock layering
11. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Clastic sedimentary rocks
Effusive eruptions
Factors of magma cooling time
Felsic - intermediate - mafic - ultramafic
12. A column of very hot rock that flows upward until it reaches the base of the lithosphere. In this model - such deep-mantle plumes form because heat rising from the Earth's core is warming rock at the base of the mantle. A possible explanation to the
Mantle plume
Limestone
Spreading rate
pahoehoe
13. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Intrusive igneous rock
Ultramafic
Dike
Transgression
14. 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 -
Tephra
Large Igneous Provinces (LIPs)
Mid-ocean ridges
Felsic
15. Two different minerals which have the same composition but have different crystal structures.
The effect of viscosity on eruptive style
Mantle plume
triple junction
Polymorphs
16. 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
Outer core
Pyroclastic flows
Lithosphere
17. 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.
Outcrop
Magnetic declination
C-horizon
Basalt
18. Mineral class; consist of metal cations bonded by oxygen anions. Examples - hematite and magnetite. Some contain a relatively high proportion of metal atoms - and thus are ore minerals.
Continental drift hypothesis
Magma's speed of flow
Granite
Oxides
19. A process occurring when sea level falls - the coast migrates seaward.
Igneous rocks
Convergent plate boundary
Regression
Bathymetry
20. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Siltstone and mudstone
Regolith
Basaltic magma
Clastic sedimentary rocks
21. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Dolostone
Seamount chains
Oxidation
Luster
22. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Rhyolitic lava flows
Residual soil
Luster
Dipole
23. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Ripples
Soil
Gabbro
Lapilli
24. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
A-horizon
Plate tectonics
E-horizon
Ripples
25. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
3.5km (2 miles)
Magma
Asthenosphere
Cement
26. Because different soil-forming processes operate at different depths - soils typically develop into these distinct zones. These zones can be arranged vertically into a soil profile.
Plates
Soil Horizons
Volcanic pipes/necks
Lower mantle
27. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Continental shelf
Metals
Sea-floor spreading
Basalt
28. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Thermal expansion
Cross beds
Laccolith
Factors classifying clastic sedimentary rocks
29. Along much of the perimeter of the Pacific Ocean - the ocean floor reaches astounding depths of 8-12km. These areas define elongate troughs - and they border volcanic arcs - the curving chains of active volcanoes.
Apparent polar-wander path
Laterite
Plutons
Deep-ocean trenches
30. 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
Siliceous rocks
Ridge-push force
Salt wedging
Xenolith
31. Some rocks develop their magnetization - their ability to produce a magnetic field - at the time that the rocks themselves formed. Such rocks - preserve a record of the Earth's magnetic field at known times in the past.
Sedimentary rocks
Paleomagnetism
rifting
The effect of gas pressure on eruptive style
32. Magma viscosity depends upon temperature - volatile content - and silica content. Hotter magma - more volatiles - and mafic magma all have less viscosity.
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33. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Peridotite
Why magma rises
Calderas
Zone of accumulation
34. The nature of Earth's magnetic field - like the familiar magnetic field around a bar magnet - has a North and South pole. The magnetic field is drawn with field lines - the paths along Which magnets would align - or charged particles would flow - if
Melts
Weathering
Dipole
Mineral crystal destruction
35. Sedimentary rocks consisting of carbon-rich relicts of plants.
Sulfides
Euhedral crystal
Organic sedimentary rocks
Continental shelf
36. 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
Outer core
Divergent plate boundary
Pyroclastic flows
Solid-state diffusion
37. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Lower mantle
Rock composition
Transform fault
Granitic composition
38. The combination of processes that separate rock or regolith from its substrate and carry it away. Involves abrasion - plucking - scouring - and dissolution - and is caused by air - water or ice.
Decompression
Erosion
Sedimentary structure
Laccolith
39. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
C-horizon
Volcanic blocks/bombs
Carbonates
Igneous rocks
40. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Regression
Granite
Earth's atmosphere
Hydrolysis
41. An envelope of gas surrounding Earth consisting of 78% nitrogen (N2) and 28% oxygen (O2) - with minor amounts 1% of argon - carbon dioxide - methane - etc. And 99% of the gas in the atmosphere lies below 50km.
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42. 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
ravertine
Redbeds
The core
Silicates
43. Highest soil horizon; consists almost entirely of organic matter and contains barely any mineral matter. Surface level has 'litter' and deeper it contains 'humus'. Part of the zone of leaching.
O-horizon
Plate tectonics
Frost wedging
Rock composition
44. 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.
Explosive eruptions
Physical weathering
Outcrop
Thermal expansion
45. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Metamorphic foliation
The core
Precipitation
Bed
46. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Strata
Chemical sedimentary rocks
Dark Silicates
Salt wedging
47. Type of igneous rock composition; composed of dark silicates and calcium-rich feldspar - referred to as mafic (magnesium and iron). Make up the ocean floor/volcanic islands.
Dolostone
Basaltic composition
Sea-floor spreading
Metamorphic foliation
48. 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.
Polymorphs
Batholiths
Seamount chains
Crystalline
49. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Geothermal gradient
Crust
Lava domes
Sedimentary structure
50. Deeper sublayer of the mantle - depth of 660km to 2900km.
Lower mantle
Agrillaceous rocks
Ridge-push force
Luster
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