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Test your basic knowledge |
Geology
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Study First
Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
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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. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Evaporites
Crust
Alloy
Superplumes
2. Chemical weathering during Which minerals dissolve into water.
E-horizon
Dissolution
Chemical sedimentary rocks
Cement
3. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Outer core
Seamount chains
Paleomagnetism
Melting
4. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Thermal expansion
Magma
Metamorphic foliation
Frost wedging
5. Sea-floor spreading proponents - Hess and others realized that in order for the circumference of the Earth to remain constant through time - ocean floor must eventually sink back into the mantle. This sinking process consumes the ocean floor between
Subduction
12km
Silicate minerals
Zone of accumulation
6. Type of volcanic eruption; takes place when water gains access to the hot rock around the magma chamber and suddenly transforms into steam - a pyroclastic eruption involving the reaction of water with magma.
Ripples
Phreatomagmatic eruptions
Crystalline igneous rocks
Convective flow
7. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Volcano
Diagenesis
Viscosity
Intrusive igneous rock
8. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Ignimbrite
Ash
Gem
9. 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.
Granitic composition
Salt wedging
Factors of magma cooling time
Color
10. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
Flood basalts
Dissolution
Streak
Cement
11. Rocks whose crystals interlock with each other.
Crystalline
Siltstone and mudstone
Jointing
Sulfates
12. 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
Ultramafic
Silicates
a'a'
Fracture and cleavage
13. 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
Plate tectonics
Magma's speed of flow
Stoping
Mid-ocean ridges
14. 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
Mantle
Thermal expansion
Rocks
Magnetic reversals
15. Sedimentary rock composed of calcite or dolomite.
Stoping
Carbonate rocks
Ignimbrite
Crystal structure
16. Weathering - erosion - transportation - deposition - and lithification.
Residual soil
Gabbro
Five steps of clastic sedimentary rock formation
Paleomagnetism
17. Physical property of a mineral; a measure of a minerals relative ability to resist scratching - and therefore represents the resistance of bonds in the crystal structure being broken. The atoms or ions in crystals of a hard mineral are more strongly
Hardness
Pangaea
Stratagraphic formation
Differential weathering
18. 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.
The effect of viscosity on eruptive style
Lithification
Rhyolitic lava flows
Igneous rocks
19. The transformation of loose sediment into solid rock.
Lithification
Sandstone
Light silicates
Chert
20. Distinguishing feature of magma; the composition of the melt reflects the composition of the solid from which it was derived. Not all magmas form from the same source rock - therefore not all magmas have the same compositions.
Quartz sandstone
O-horizon
Laterite
Source rock composition
21. When different rocks in an outcrop undergo weathering at different rates.
Differential weathering
Hot-spot track
Earth's atmosphere
Grain sizes
22. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Stoping
atmospheres (atm)
Plates
Paleopole
23. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Pangaea
Saprolite
Loam
Granite
24. 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
Melting
Tephra
Depositional environment
E-horizon
25. The boundary between two beds is a bedding plane; several beds constitute this structure.
Root wedging
Spreading rate
Strata
The core
26. 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.
Divergent plate boundary
Rock layering
Redbeds
Biomineralization
27. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Rock-forming silicate minerals
Halides
E-horizon
Depositional environment
28. 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
Marine magnetic anomaly
Light silicates
Why magma rises
Crystal lattice
29. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Abyssal plains
Tuff
Ridge-push force
Conchoidal fractures
30. 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.
Continental shelf
Volcanic blocks/bombs
Plutons
Sulfides
31. 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.
Bedrock
Rock composition
Arkose
Pyroclastic debris
32. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Convective flow
Magnetic reversals
Explosive eruptions
Basalt
33. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Chert
Basaltic magma
ravertine
collision
34. Cause of melting; magma can also form at locations where chemicals called volatiles mix with hot mantle rock. Elements such as water and carbon dioxide mix with hot rock - helping to break chemical bonds - so that if you add volatiles to a solid - ho
Granite
Volatiles
Silicate minerals
Magma mixing
35. 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.
A-horizon
Color
Silicate minerals
Sedimentary rocks
36. Type of volcano; broad and slightly domed - primarily made of basaltic lava - large and erupt large volumes of lava. Form from either low viscosity basaltic lava or from large pyroclastic sheets.
Shield volcano
Batholiths
Zone of accumulation
Composite cone (stratovolcano)
37. Rock formations still attached to the Earth's crust.
Continental rift
Slab-pull force
Bedrock
Cementation
38. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
The effect of gas pressure on eruptive style
Factors classifying clastic sedimentary rocks
Arkose
Xenolith
39. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Peridotite
Grain sizes
C-horizon
Rock layering
40. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
The effect of viscosity on eruptive style
Luster
Frost wedging
Abyssal plains
41. Physical features of the land surface represented by changes in elevation.
Sulfides
Transition zone
Topography
Superplumes
42. 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 -
Polymorphs
Euhedral crystal
Large Igneous Provinces (LIPs)
Mid-ocean ridges
43. Process occurring after sediment has been compacted - can then be bounded together to make coherent sedimentary rock. Binding material consists of minerals (commonly quartz or calcite).
Bedrock
Melting
Rocks
Cementation
44. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Lava tube
Jointing
Area of igneous activity
Strata
45. The supercontinent; existence proposed by Wegener - suggested that the supercontinent later fragmented into separate continents that then drifted apart - moving slowly to their present positions.
Pangaea
Lava tube
Redbeds
Flood basalts
46. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
12km
Basalt
Peridotite
Sedimentary structure
47. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Specific gravity
Weathering
Chert
Pyroclastic flows
48. 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.
Lower mantle
Apparent polar-wander path
Relative plate velocity
Salt wedging
49. 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.
Chemical weathering
Mafic
Fracture zones
Sea-floor spreading
50. 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.
Magnetic declination
Heat transfer
Oxides
Lapilli
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