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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. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Marine magnetic anomaly
Alloy
The effect of the environment on eruptive style
Inner core
2. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Reason for Earth's internal heat
Viscosity
Frost wedging
Arkose
3. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Superplumes
Hydrolysis
Plutons
Rocks
4. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Transported soil
Geothermal gradient
Biomineralization
Gabbro
5. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Superplumes
Facets
Sill
Fracture zones
6. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Topography
Redbeds
Regression
Sedimentary structure
7. 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.
The effect of viscosity on eruptive style
Soil erosion
Zone of accumulation
Assimilation
8. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Conchoidal fractures
Hydrosphere
E-horizon
Lithification
9. 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.
The effect of the environment on eruptive style
Paleomagnetism
Melts
Siltstone and mudstone
10. A place where three plate boundaries intersect at a point.
Gabbro
Limestone
Mantle
triple junction
11. Two different minerals which have the same composition but have different crystal structures.
Mid-ocean ridges
Polymorphs
Ignimbrite
Silicate minerals
12. 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.
Rock composition
Marine magnetic anomaly
Quartz sandstone
Ultramafic
13. 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
Rock texture
Mantle plume
Sedimentary structure
Dunes
14. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Composite cone (stratovolcano)
Apparent polar-wander path
Effusive eruptions
Peridotite
15. 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.
Metals
Composite cone (stratovolcano)
Rocks
Elemental composition of Earth
16. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Gem
Strata
Thermal expansion
Regolith
17. Tree roots that grow into joints can push those joints open in this process.
Lava
Root wedging
Continental rift
Clastic sedimentary rocks
18. 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.
Native metals
Reason for Earth's internal heat
Plates
Relative plate velocity
19. The removal of soil by running water or by wind.
Magnetic inclination
Cinder cone
Soil erosion
Crystal structure
20. 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
Soil Horizons
Volcano
Basaltic magma
21. 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.
Large Igneous Provinces (LIPs)
Biochemical sedimentary rocks
Dipole
650-1100 degrees C
22. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Factors classifying clastic sedimentary rocks
Fracture and cleavage
Factors of magma cooling time
Convective flow
23. An insulated - tunnel-like conduit through which lava moves within a flow.
Silicates
Dunes
Lava tube
Biomineralization
24. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Saprolite
Diagenesis
Organic chemicals
Chemical weathering
25. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Compaction
Halides
Magnetic declination
Columnar jointing
26. On a gem are the ground and polished surfaces made with a certain type of machine.
Facets
Magma mixing
Glass
Volcanic blocks/bombs
27. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Ridge-push force
Ultramafic
Magma mixing
Extrusive igneous rock
28. A process occurring when sea level falls - the coast migrates seaward.
Depositional environment
a'a'
Regression
Hydrosphere
29. Places where intrusive igneous rock creates tabular intrusions cutting across rock that does not have layering - this nearly vertical - wall-like tabular intrusions is formed. Cut across layering within the earth.
Organic chemicals
Columnar jointing
Dike
Melting
30. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
collision
Arkose
Rock-forming silicate minerals
Andesitic lava flows
31. A mineral's growth that is uninhibited - has well-formed crystal faces.
Bedrock
Mantle plume
Euhedral crystal
Arkose
32. The process by which sediment settles out of the transporting medium.
Soil
Continental drift evidence
Deposition
Xenolith
33. Core division; from a depth of 5155km down to Earth's center at 6371km. A radius of about 1220km - is solid iron-nickel alloy - can reach temperature of 4700 degrees C. Solid in nature because of subjection to greater pressure - keeps atoms from wand
pahoehoe
Inner core
Transform fault
Sandstone
34. 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.
Rock-forming silicate minerals
Oxides
Streak
Superplumes
35. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Crystalline igneous rocks
Granitic magma
Organic chemicals
The effect of the environment on eruptive style
36. A rock made of solid mass of glass - or of tiny crystals surrounded by glass. Reflect light as glass does and tend to break conchoidally. Examples - obsidian - tachylite - pumice.
Glassy igneous rocks
Mantle plume
Dissolution
Stratagraphic formation
37. A sediment-filled depression; in an area where the lithosphere has subsided.
Conchoidal fractures
Lapilli
Sedimentary Basins
Sedimentary rocks
38. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Granitic composition
Sea-floor spreading
Lapilli
Granitic magma
39. 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
Sandstone
Intrusive igneous rock
Crust
40. 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
Salt wedging
Loam
Decompression
41. 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.
Glass
Factors classifying clastic sedimentary rocks
Zone of leaching
Sulfates
42. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Biomineralization
Calderas
Metals
The effect of gas pressure on eruptive style
43. Layering in sedimentary rocks.
Graded bed
650-1100 degrees C
Bedding
Pyroclastic debris
44. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Seamount chains
Basaltic composition
Specific gravity
Chemical weathering
45. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Rock-forming silicate minerals
Continental rift
Geothermal gradient
Subduction
46. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Sea-floor spreading
atmospheres (atm)
Stoping
Plutons
47. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Factors classifying clastic sedimentary rocks
Continental drift evidence
Euhedral crystal
Regression
48. The crust moves away from the Mid-Atlantic Ridge axis at a rate of 1cm per year. This velocity of sea-floor spreading is determined by the relationship between the paleomagnetic anomaly-stripe's width and the reverse polarity duration - the data reve
Inner core
Hydrosphere
Spreading rate
Dike
49. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
3.5km (2 miles)
Magnetic inclination
Andesitic lava flows
Conchoidal fractures
50. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
Special properties of minerals
Continental rift
Ultramafic
Why magma rises
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