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Test your basic knowledge |
Geology
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Study First
Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
If you are not ready to take this test, you can
study here
.
Match each statement with the correct term.
Don't refresh. All questions and answers are randomly picked and ordered every time you load a test.
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 sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Mafic
Phreatomagmatic eruptions
C-horizon
2. 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
Conglomerate
atmospheres (atm)
Calderas
3. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Crystal lattice
Sea-floor spreading
Metamorphic foliation
collision
4. A place where three plate boundaries intersect at a point.
triple junction
Explosive eruptions
Flood basalts
Asthenosphere
5. 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.
Explosive eruptions
C-horizon
Extrusive igneous rock
Sedimentary rocks
6. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Volcano
The effect of the environment on eruptive style
The effect of viscosity on eruptive style
Lava domes
7. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Depositional environment
Abyssal plains
Lapilli
Superplumes
8. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Gem
Thermal expansion
Factors classifying clastic sedimentary rocks
Symmetry
9. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Metamorphic rocks
Fracture and cleavage
Streak
Superplumes
10. Sedimentary rock composed of calcite or dolomite.
Zone of leaching
Magma mixing
Carbonate rocks
Oxides
11. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
triple junction
Sandstone
Precipitation
pahoehoe
12. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Fracture and cleavage
Diagenesis
Basaltic lava flows
Plates
13. 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.
Physical weathering
B-horizon
Subduction
Effusive eruptions
14. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Soil erosion
Euhedral crystal
Andesitic lava flows
Magnetic declination
15. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Sedimentary structure
Grain sizes
Why magma rises
Metals
16. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
atmospheres (atm)
Glassy igneous rocks
Basalt
Diagenesis
17. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Granitic magma
Inner core
Color
Felsic
18. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Intrusive igneous rock
Strata
E-horizon
Sill
19. Contributes to formation of soil; occurs when rainwater percolates through the debris and carries dissolved ions and clay flakes downward - This is the region where the downward transport occurs.
Zone of leaching
Chemical sedimentary rocks
Columnar jointing
Crystal structure
20. A distinctive sequence of strata traced across a fairly large region. For example - a region may contain a succession of alternating sandstone and shale beds deposited by rivers - overlain by beds of marine limestone deposited later.
Granitic composition
Stratagraphic formation
Cementation
Dipole
21. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Paleomagnetism
Factors of magma cooling time
Mid-ocean ridges
Chemical weathering
22. 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
Hydrolysis
Magnetic declination
Magma mixing
Metamorphic foliation
23. Created from preexisting rocks which undergo changes - such as the growth of new minerals in response to pressure and heat - and/or as a result of squashing - stretching - or shear.
Bed
Jointing
Metamorphic rocks
Continental drift hypothesis
24. A term used for all the physical - chemical - and biological processes that transform sediment into sedimentary rock and that alter characteristics of sedimentary rock one the rock has formed.
Weathering
Sedimentary rocks
Diagenesis
Lithification
25. A single - continuous (uninterrupted) piece of a crystalline solid bounded by flat surfaces called crystal faces that grew naturally as the mineral formed. Come in a variety of shapes - cubes - trapezoids - pyramids - octahedrons - hexagonal columns
Crystalline igneous rocks
Continental shelf
Crystal
Hydration
26. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Basalt
Carbonate rocks
Euhedral crystal
Frost wedging
27. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Fracture zones
Crystal habit
Granitic magma
Slab-pull force
28. Sedimentary rock composed of quartz.
Assimilation
Volcanic pipes/necks
Siliceous rocks
The core
29. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Magma's speed of flow
Diagenesis
Cross beds
Transform fault
30. Physical property of a mineral; different minerals fracture in different ways - depending on the internal arrangement of atoms. If a mineral breaks to form distinct planar surfaces that have a specific orientation in relation to the crystal structure
pahoehoe
Magma
Fumerolic mineralization
Fracture and cleavage
31. 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.
Compaction
Physical weathering
Earth's atmosphere
Rock-forming silicate minerals
32. Process where new divergent boundaries form when a continent splits and separates into two continents.
Spreading rate
Rock-forming silicate minerals
rifting
Color
33. 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.
Granite
Continental drift hypothesis
Laterite
Assimilation
34. 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.
Inner core
Sandstone
Topography
Cross beds
35. 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.
Erosion
Metamorphic rocks
Decompression
Slab-pull force
36. The Earth radiated heat into space and slowly cooled. Eventually - the early formed sea of lava solidified and formed igneous rock. The cumulative effect of radioactivity has been sufficient to slow the cooling of the planet and subsequently allow fo
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37. Chemical weathering during Which minerals dissolve into water.
Outer core
Sandstone
Transgression
Dissolution
38. A plate boundary at which one plate slips along the side of another plate. No new plate is formed and no old plate is consumed. But the grinding between the plates generates frequent and destructive earthquakes.
Transform plate boundary
Quartz sandstone
atmospheres (atm)
Dunes
39. 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.
Solid-state diffusion
Rock-forming silicate minerals
Subduction
Deep-ocean trenches
40. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Fumerolic mineralization
Conglomerate
Stoping
Transform plate boundary
41. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Magma mixing
Arkose
Quartz sandstone
Volatiles
42. On a gem are the ground and polished surfaces made with a certain type of machine.
Facets
Deep-ocean trenches
Metals
Fragmental igneous rocks
43. 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
Soil Horizons
Effusive eruptions
Granitic magma
Outer core
44. 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
Silicate minerals
Salt wedging
Volatiles
Superplumes
45. The display of the pattern of atoms or ions within a mineral. Meaning that the shape of one part of a mineral is a mirror image of the shape of another part.
Pyroclastic flows
Ripples
Symmetry
Cement
46. 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
Felsic - intermediate - mafic - ultramafic
Turbidite
Dipole
Sedimentary Basins
47. 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.
Soil Horizons
Regression
Factors of magma cooling time
Biochemical sedimentary rocks
48. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Transported soil
12km
Batholiths
Lava tube
49. Tree roots that grow into joints can push those joints open in this process.
Calderas
Earth's atmosphere
pahoehoe
Root wedging
50. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Crystalline igneous rocks
Volcanic blocks/bombs
Convective flow
Lapilli