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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. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Plates
Mid-ocean ridges
Transform plate boundary
Erosion
2. 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
Crystal
Silicates
Fumerolic mineralization
Rock composition
3. A process occurring when sea level falls - the coast migrates seaward.
Granite
Ripples
Regression
Mineral crystal destruction
4. A solid in which atoms are not arranged in an orderly pattern. Forms when a liquid freezes so fast that atoms do not have time to organize into an orderly pattern.
B-horizon
a'a'
Glass
Paleopole
5. 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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6. Sublayer of the mantle - depth of 660km.
3.5km (2 miles)
Symmetry
Assimilation
Upper mantle
7. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Hot spots
Basalt
Paleomagnetism
Sandstone
8. Physical features of the land surface represented by changes in elevation.
Hydrolysis
Topography
B-horizon
Continental drift evidence
9. The resistance to flow of magma. Reflects its distinct silica content - for silica tends to polymerize - meaning it links up to form long - chainlike molecules whose presence slows down the flowing ability of magma. Thus felsic magmas flow less easil
Soil
Transition zone
Root wedging
Viscosity
10. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
Rock texture
Heat transfer
Xenolith
pahoehoe
11. 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.
Granite
Quartz sandstone
Factors of magma cooling time
Divergent plate boundary
12. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Rhyolitic lava flows
Factors classifying clastic sedimentary rocks
Felsic - intermediate - mafic - ultramafic
ravertine
13. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Dolostone
Volcanic pipes/necks
Continental shelf
Convective flow
14. Magma is less dense than surrounding rock - and thus is buoyant. Magma is less dense both because rock expands as it melts and because magma tends to contain smaller proportions of heavy elements. Also - magma rises because the weight of overlying ro
B-horizon
Rhyolitic lava flows
Why magma rises
Organic chemicals
15. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Evaporites
Magnetic declination
Chemical weathering
O-horizon
16. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Hydrolysis
Area of igneous activity
Ripples
Rock composition
17. 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.
Crystal structure
Effusive eruptions
Oxidation
Fragmental igneous rocks
18. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Assimilation
Pyroclastic debris
Continental shelf
Dissolution
19. 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.
Metamorphic foliation
Crystal structure
Heat transfer
Carbonate rocks
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.
Specific gravity
Intrusive igneous rock
Hydration
Regolith
21. 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.
Sea-floor spreading
Lava tube
Composite cone (stratovolcano)
Biochemical sedimentary rocks
22. 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.
Mafic
Fumerolic mineralization
Crystal structure
Magnetic declination
23. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Continental drift evidence
Graded bed
Hot-spot track
Paleopole
24. Mineral group; olivine group - pyroxene group - amphibole group.
E-horizon
Shield volcano
Dark Silicates
Lava domes
25. Tree roots that grow into joints can push those joints open in this process.
Root wedging
Rock layering
Asthenosphere
Magnetic reversals
26. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Topography
Bedding
Metals
Continental drift hypothesis
27. Farther down from a zone of leaching - new mineral crystals precipitate directly out of the water or form when the water reacts with debris - this the region where the new minerals and clay collect.
Bedding
Zone of accumulation
Magma
Peridotite
28. 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.
Convective flow
Erosion
Silicate minerals
12km
29. Physical property of a mineral; results from the way a mineral interacts with light. A mineral absorbs certain wavelengths - so the color seen represents the color wavelengths the mineral did not absorb.
Seamount chains
Deposition
Metals
Color
30. 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
Convective flow
Turbidite
Outer core
Glassy igneous rocks
31. 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
Redbeds
B-horizon
Pangaea
32. Layering in sedimentary rocks.
Apparent polar-wander path
Jointing
Factors classifying clastic sedimentary rocks
Bedding
33. Refers to the proportions of different chemicals making up the rock - and thus the proportion chemicals affects the proportions of different minerals constituting the rock.
Asthenosphere
Basaltic magma
Lapilli
Rock composition
34. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Alloy
Organic chemicals
Gem
Ignimbrite
35. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Cement
ravertine
Graded bed
Sea-floor spreading
36. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
ravertine
Cross beds
Gabbro
Silicate minerals
37. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Regolith
Ultramafic
triple junction
Rhyolitic lava flows
38. Molten rock that has flowed out onto Earth's surface.
Loam
Volcano
Lava
Grain sizes
39. Physical property of a mineral; refers to the color of a powder produced by pulverizing the mineral. Provides a fairly reliable clue to the mineral's identity - since the color of the mineral powder tends to be less variable than the color of the who
Biomineralization
Continental drift evidence
Streak
Columnar jointing
40. Factors; the depth of the intrusion - the deeper - the more slowly it cools. The shape and size of a magma body - the greater the surface area - the faster it cools. The presence of circulating groundwater - water passing through cools magma faster.
Turbidity current
Factors of magma cooling time
Frost wedging
Intermediate
41. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Stoping
Sulfates
Alloy
Why magma rises
42. A place where three plate boundaries intersect at a point.
Depositional environment
Plate tectonics
triple junction
Shield volcano
43. 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.
Volcanic blocks/bombs
Thermal expansion
Compaction
Fumerolic mineralization
44. Theory confirmed by 1968 - geologists had developed the complete model of continental drift - sea-floor spreading - and subduction. Within this model - Earth's lithosphere consists of about 20 distinct pieces - or plates - that move relative to each
Precipitation
Hot-spot track
Plate tectonics
Silicate minerals
45. 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.
Apparent polar-wander path
Continental drift hypothesis
Flood basalts
B-horizon
46. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Sulfates
Subsidence
Magnetic declination
Biomineralization
47. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Magma's speed of flow
Hydrolysis
Ash
Dolostone
48. 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
3.5km (2 miles)
Fractional crystallization
Cinder cone
49. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Frost wedging
650-1100 degrees C
Glass
collision
50. 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
Polymorphs
Magma mixing
Special properties of minerals
Metamorphic foliation