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Test your basic knowledge |
Geology
Start Test
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. 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.
Volcanic blocks/bombs
Biochemical sedimentary rocks
Paleomagnetism
Rock layering
2. 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.
Plates
Soil
Turbidite
Oxides
3. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Chemical weathering
Cinder cone
Dolostone
Granite
4. 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.
O-horizon
pahoehoe
B-horizon
Ignimbrite
5. The speed of the movements of the plates with respect to the speed of the other plates' movements. Absolute plate velocity is a measure of the movement of any plates relative to a fixed point in the mantle.
Ash
Relative plate velocity
Igneous rocks
Topography
6. 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
Silicate minerals
Melting
Basaltic magma
7. The record of paleomagnetism revealed that the location of Earth's magnetic poles had been changing through geologic time. This 'wandering' meant that Earth's magnetic poles do not move with respect to fixed continents. Rather - continents move relat
Clastic
a'a'
Siliceous rocks
Apparent polar-wander path
8. Soil section below the O-horizon - humus has decayed further and has mixed with mineral grains (clay - silt - and sand). Water percolating through this horizon causes chemical weathering reactions to occur and produces ions in solution and new clay m
Basaltic magma
A-horizon
Grain sizes
Redbeds
9. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Coal
Granite
Subsidence
Sulfates
10. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Stoping
ravertine
Rocks
Basaltic lava flows
11. 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.
Magma's speed of flow
Fragmental igneous rocks
Stoping
Special properties of minerals
12. 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.
650-1100 degrees C
Clastic sedimentary rocks
Marine magnetic anomaly
Jointing
13. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Cross beds
Partial melting
Crystal lattice
Redbeds
14. A type of soil consisting of about 10-30% clay and the rest silt and sand. Pores remain between grains so that water and air can pass through and roots can easily penetrate.
Tuff
Loam
Carbonate rocks
Cement
15. Deeper sublayer of the mantle - depth of 660km to 2900km.
Lower mantle
pahoehoe
Loam
Stratagraphic formation
16. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Soil Horizons
Magma mixing
Fractional crystallization
Native metals
17. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Decompression
Fracture and cleavage
Salt wedging
Crystalline igneous rocks
18. Sedimentary rock composed of calcite or dolomite.
Rhyolitic lava flows
Lithosphere
Carbonate rocks
Subduction
19. Mineral group; olivine group - pyroxene group - amphibole group.
Outcrop
Dark Silicates
Spreading rate
Rock layering
20. Times when the Earth's magnetic field flips from normal to reversed polarity - or vice versa. When the Earth has reversed polarity - the south magnetic pole lies near the north geographic pole - and the north magnetic pole lies near the south geograp
Magnetic reversals
Organic chemicals
E-horizon
Transform fault
21. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Divergent plate boundary
Halides
Lithification
Stoping
22. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Laccolith
Convective flow
Apparent polar-wander path
Hot-spot track
23. 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
Geothermal gradient
Turbidite
Zone of leaching
Divergent plate boundary
24. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Explosive eruptions
Continental shelf
Intermediate
Clastic sedimentary rocks
25. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Lava tube
Deposition
Transgression
Pyroclastic flows
26. A mineral's growth that is uninhibited - has well-formed crystal faces.
Hot spots
Coal
Silicate minerals
Euhedral crystal
27. 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.
Composite cone (stratovolcano)
Deep-ocean trenches
Paleopole
Volcanic blocks/bombs
28. Layering in metamorphic rocks.
A-horizon
Soil Horizons
Metamorphic foliation
collision
29. 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.
Erosion
collision
Xenolith
Basaltic composition
30. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Erosion
Columnar jointing
Special properties of minerals
Clastic
31. 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
Ignimbrite
Decompression
Biomineralization
32. Molten rock beneath Earth's surface.
Magma
Soil
Intermediate
Arkose
33. 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.
Compaction
Glass
Assimilation
Special properties of minerals
34. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Ash
Bedding
Metals
Ignimbrite
35. Form when solid materials become hot and transform into liquid - example - molten rock.
Crystalline igneous rocks
Crystalline
Melts
Volatiles
36. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Lava
Pyroclastic flows
Composite cone (stratovolcano)
Sedimentary rocks
37. 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.
Area of igneous activity
Frost wedging
Diagenesis
Streak
38. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Sedimentary structure
Compaction
Zone of accumulation
Conchoidal fractures
39. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Intermediate
Topography
Oxidation
ravertine
40. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Assimilation
Erosion
650-1100 degrees C
Hydrosphere
41. Two different minerals which have the same composition but have different crystal structures.
Polymorphs
O-horizon
Rhyolitic lava flows
Assimilation
42. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Transition zone
Rhyolitic lava flows
Large Igneous Provinces (LIPs)
Pyroclastic debris
43. 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.
Transported soil
Conglomerate
Fumerolic mineralization
Compaction
44. 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.
Continental drift evidence
Native metals
Elemental composition of Earth
Fracture zones
45. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Peridotite
Fractional crystallization
Volcanic pipes/necks
Dissolution
46. A place where three plate boundaries intersect at a point.
Convective flow
triple junction
Magnetic anomaly
Redbeds
47. Sublayer of the mantle - depth of 660km.
Convective flow
Upper mantle
Silicate minerals
Granitic magma
48. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Pyroclastic debris
Granitic magma
Outcrop
Siliceous rocks
49. Process where new divergent boundaries form when a continent splits and separates into two continents.
Fragmental igneous rocks
Mafic
Marine magnetic anomaly
rifting
50. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Sill
Xenolith
Depositional environment
Outcrop