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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. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Caliche
Transform fault
Redbeds
O-horizon
2. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Melting
Geothermal gradient
Conchoidal fractures
Laccolith
3. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Magma's speed of flow
Turbidite
Plate tectonics
Volatiles
4. 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.
Subduction
Magma
Laterite
Fumerolic mineralization
5. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Paleopole
Native metals
Superplumes
Relative plate velocity
6. 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.
Frost wedging
Paleomagnetism
Soil erosion
Divergent plate boundary
7. 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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8. Aggregates of mineral crystals or grains - and masses of natural glass; a coherent - naturally occurring solid - consisting of an aggregate of minerals or a mass of glass.
Basaltic magma
Rocks
Turbidity current
Fracture zones
9. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Hydrolysis
Batholiths
Factors of magma cooling time
Composite cone (stratovolcano)
10. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Rock composition
Transported soil
Seamount chains
Marine magnetic anomaly
11. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
12km
Limestone
pahoehoe
Why magma rises
12. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Alloy
Laterite
Pyroclastic flows
Phreatomagmatic eruptions
13. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
ravertine
Soil Horizons
Sea-floor spreading
Evaporites
14. 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.
Silicate minerals
Cross beds
Five steps of clastic sedimentary rock formation
Regolith
15. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Rock composition
Halides
Stoping
16. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Subduction
Slab-pull force
Loam
Basaltic composition
17. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Superplumes
Flood basalts
Basaltic magma
Quartz sandstone
18. 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
Biomineralization
Residual soil
Viscosity
Native metals
19. Form when solid materials become hot and transform into liquid - example - molten rock.
Melts
Polymorphs
Jointing
Continental rift
20. Layering in sedimentary rocks.
Magnetic anomaly
Bedding
Stratagraphic formation
Erosion
21. Mineral group; olivine group - pyroxene group - amphibole group.
Dark Silicates
Bathymetry
Bedding
Cementation
22. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
The effect of gas pressure on eruptive style
Magnetic inclination
Solid-state diffusion
Tephra
23. A distinctive sequence of strata traced across a fairly large region. For example - a region may contain a succession of alternating sandstone and shale beds deposited by rivers - overlain by beds of marine limestone deposited later.
Apparent polar-wander path
Stratagraphic formation
Factors classifying clastic sedimentary rocks
Fracture zones
24. 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.
Relative plate velocity
Metamorphic foliation
ravertine
Rock texture
25. 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
Melts
Saprolite
Mantle plume
Chemical sedimentary rocks
26. 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
collision
Felsic - intermediate - mafic - ultramafic
Halides
Flood basalts
27. Created from preexisting rocks which undergo changes - such as the growth of new minerals in response to pressure and heat - and/or as a result of squashing - stretching - or shear.
Metamorphic rocks
Why magma rises
E-horizon
Sedimentary Basins
28. 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.
Evaporites
Pangaea
Crystal habit
Arkose
29. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Streak
Metals
Crystal lattice
Ignimbrite
30. Sedimentary rock composed of quartz.
Weathering
Siliceous rocks
Conchoidal fractures
Pangaea
31. 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
Sandstone
Sedimentary Basins
Magnetic reversals
Magnetic declination
32. Process where new divergent boundaries form when a continent splits and separates into two continents.
rifting
Sulfides
Elemental composition of Earth
Silicate minerals
33. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Transported soil
Grain sizes
Native metals
Organic sedimentary rocks
34. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Continental drift hypothesis
Bed
Reason for Earth's internal heat
Soil Horizons
35. Tree roots that grow into joints can push those joints open in this process.
Root wedging
Factors classifying clastic sedimentary rocks
Magma's speed of flow
Granite
36. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Outer core
Root wedging
Paleopole
a'a'
37. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Sedimentary rocks
Oxides
Granite
Mantle plume
38. When silt and clay accumulate in the flat areas bordering a stream - lagoon - or delta - the silt when lithified becomes this type of sediment. And the mud - when lithified - becomes another type of sediment - also known as shale.
Transgression
Evaporites
Oxides
Siltstone and mudstone
39. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Elemental composition of Earth
triple junction
Regolith
Igneous rocks
40. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
triple junction
Lithosphere
Intrusive igneous rock
Columnar jointing
41. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Gem
Frost wedging
Deep-ocean trenches
Lapilli
42. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Coal
Agrillaceous rocks
Ridge-push force
Sulfates
43. Type of volcano; built from ejected lava fragments - cone shaped piles of tephra - steep slope angle - smaller in size - frequently occur in groups - deep craters.
Chemical sedimentary rocks
Cinder cone
The effect of gas pressure on eruptive style
Dunes
44. 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.
Basaltic composition
Subsidence
Conglomerate
Granite
45. Process occurring in arid climates - dissolved salt in groundwater precipitates and grows as crystals in open pore spaces in rocks. This process pushes apart the surrounding grains and so weakens the rock that when exposed to wind or rain - the rock
collision
Salt wedging
Polymorphs
Crystal lattice
46. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Subsidence
Intrusive igneous rock
Limestone
Viscosity
47. 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.
Dipole
Fumerolic mineralization
Continental drift hypothesis
Chemical sedimentary rocks
48. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Seamount chains
Continental drift evidence
Granite
Organic sedimentary rocks
49. Center of the Earth - consists mainly of iron alloy.
The core
Ultramafic
Batholiths
Lithosphere
50. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Effusive eruptions
Silicate minerals
Soil erosion
Polymorphs