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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. 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.
12km
Soil Horizons
Regression
Batholiths
2. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Basalt
Phreatomagmatic eruptions
Redbeds
Effusive eruptions
3. 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
atmospheres (atm)
Continental shelf
Organic chemicals
Magnetic reversals
4. The transformation of loose sediment into solid rock.
Silicate minerals
Convective flow
Lithification
Physical weathering
5. 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.
Chemical weathering
Fracture zones
Crystal structure
Frost wedging
6. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
The core
Metals
Oxides
Inner core
7. 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.
Basaltic composition
Felsic - intermediate - mafic - ultramafic
Silicate minerals
Transform plate boundary
8. 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
Hydrolysis
Basaltic lava flows
Asthenosphere
9. Type of volcanic eruption; pyroclastic - produce clouds and avalanches of pyroclastic debris. Gas expands in the rising magma - cannot escape. The pressure becomes so great that it blasts the lava - and volcanic rock - out of the volcano.
Rocks
Explosive eruptions
Sandstone
Rock-forming silicate minerals
10. 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
Biochemical sedimentary rocks
Mantle plume
Rocks
Quartz sandstone
11. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Factors classifying clastic sedimentary rocks
Volcano
Transported soil
Precipitation
12. A fine spray of lava instantly freezes to form fine particles of glass.
Fractional crystallization
Turbidity current
Ash
Halides
13. 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
Silicates
Geothermal gradient
B-horizon
Magma's speed of flow
14. Sedimentary rocks consisting of carbon-rich relicts of plants.
Organic sedimentary rocks
Carbonate rocks
Asthenosphere
Turbidity current
15. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Gabbro
Hot spots
Hydrosphere
Solid-state diffusion
16. 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
Magma mixing
Hydration
Plutons
Ash
17. Forms a 2885-km-thick layer surrounding the core. In terms of volume - it is the largest part of the Earth. It consists entirely of ultramafic rock - peridotite.
Strata
Mantle
Magnetic reversals
Caliche
18. Type of soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
Laterite
Depositional environment
Mineral crystal destruction
triple junction
19. 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.
Bed
Fracture zones
Pangaea
Upper mantle
20. Mineral class; consist of a metal cation bonded to the anionic group. Many form by precipitation out of water at or near the Earth's surface. Example - gypsum.
Erosion
Ultramafic
Sulfates
Heat transfer
21. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Turbidity current
Continental shelf
Columnar jointing
Weathering
22. 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.
Specific gravity
Basalt
Hydrosphere
Color
23. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Dolostone
Convective flow
Effusive eruptions
Streak
24. 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
Siltstone and mudstone
Calderas
Apparent polar-wander path
Geothermal gradient
25. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Halides
Relative plate velocity
Saprolite
Outer core
26. Forms when clots of lava fly into the air in lava fountains and then freeze to form solid chunks before hitting the ground. Some forms when the explosion of a volcano shatters preexisting rock and ejects the fragments over the countryside.
Magnetic inclination
Lithification
Bed
Pyroclastic debris
27. The most common minerals in the Earth. Contain silica (SiO2) mixed in varying proportions with other elements (typically iron - magnesium - aluminum - calcium - potassium - and sodium).
Cement
Spreading rate
Mafic
Silicate minerals
28. 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
Fissure eruptions/lava plateaus
Volatiles
Sea-floor spreading
Crystal lattice
29. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Decompression
Sedimentary structure
Carbonates
Pangaea
30. Places with particularly voluminous quantities of magma erupting or intruding.
Gabbro
Paleopole
The effect of the environment on eruptive style
Large Igneous Provinces (LIPs)
31. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Glassy igneous rocks
Alloy
pahoehoe
Intrusive igneous rock
32. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
Source rock composition
Erosion
Decompression
Redbeds
33. The base of the soil profile; consists of material derived from the substrate that's been chemically weathered and broken apart - but has not yet undergone leaching or accumulation.
Precipitation
Slab-pull force
Sedimentary Basins
C-horizon
34. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Metamorphic foliation
Chemical sedimentary rocks
Asthenosphere
Intermediate
35. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Gabbro
Gem
Rock composition
Caliche
36. Rocks which develop when hot molten rock cools and freezes solid.
Tuff
Ultramafic
Igneous rocks
The effect of the environment on eruptive style
37. Refers to the arrangement of grains in a rock; that is - the way the grains connect each other and whether inequant grains are aligned parallel to one another.
Rock texture
Transform fault
Root wedging
Crystal structure
38. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Crystal lattice
Oxides
Jointing
Lapilli
39. 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.
Oxidation
Magnetic declination
Convective flow
Bathymetry
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.
Convective flow
Abyssal plains
Stoping
12km
41. 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
Biochemical sedimentary rocks
Symmetry
Upper mantle
Outer core
42. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Caliche
Arkose
Pangaea
Alloy
43. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Chemical weathering
Clastic
Sedimentary Basins
Lower mantle
44. 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.
Weathering
Volcanic blocks/bombs
Composite cone (stratovolcano)
Hot spots
45. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Polymorphs
Hydration
Transform fault
Subsidence
46. The injection of magma within the magma chamber and conduit generates an outward pressure within the volcano. The presence of gas within the magma increases this pressure - as gas expands greatly as it rises toward the Earth's surface. Rhyolitic and
Biochemical sedimentary rocks
The effect of gas pressure on eruptive style
Pangaea
Mid-ocean ridges
47. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Intrusive igneous rock
Metamorphic rocks
Transported soil
Laccolith
48. The removal of soil by running water or by wind.
Luster
Erosion
Soil erosion
3.5km (2 miles)
49. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Partial melting
Asthenosphere
Rock layering
ravertine
50. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Pyroclastic debris
Hydrosphere
Ridge-push force
Volcano