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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. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Seamount chains
Rock-forming silicate minerals
Relative plate velocity
Ripples
2. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Zone of leaching
Alloy
Regolith
Granitic magma
3. 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
Why magma rises
Oxides
Lithification
4. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Cement
Turbidity current
Halides
Specific gravity
5. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Light silicates
Sill
Lithification
Marine magnetic anomaly
6. 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.
Sulfides
Specific gravity
Sea-floor spreading
Limestone
7. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
O-horizon
Arkose
Volatiles
Hydration
8. Sedimentary rock composed of clay.
Turbidity current
Glass
Continental shelf
Agrillaceous rocks
9. 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.
Crystal lattice
Siltstone and mudstone
Inner core
Mineral crystal destruction
10. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Clastic
Graded bed
Native metals
Euhedral crystal
11. 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
Metamorphic foliation
Hardness
Silicate minerals
12km
12. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Specific gravity
Caliche
Dolostone
Rocks
13. Tree roots that grow into joints can push those joints open in this process.
The effect of viscosity on eruptive style
Continental drift hypothesis
Root wedging
Partial melting
14. 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.
Carbonate rocks
Andesitic lava flows
Glass
Mineral crystal destruction
15. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Continental shelf
Ignimbrite
Deposition
Magma's speed of flow
16. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Volcanic blocks/bombs
Plates
Gem
Gabbro
17. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Rock composition
Conchoidal fractures
Native metals
Turbidite
18. When different rocks in an outcrop undergo weathering at different rates.
Metals
Differential weathering
Why magma rises
Fracture and cleavage
19. 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.
Rhyolitic lava flows
Weathering
Erosion
Mid-ocean ridges
20. 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.
Fracture and cleavage
Cinder cone
650-1100 degrees C
Basaltic magma
21. Sedimentary rock composed of quartz.
Fracture and cleavage
Heat transfer
Volatiles
Siliceous rocks
22. Volcanoes that exist as isolated points and appear to be independent of movement at a plate boundary - hot-spot volcanoes. Mostly are located on the interior of plates - away from boundaries.
Intrusive igneous rock
B-horizon
Quartz sandstone
Hot spots
23. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Magma
Grain sizes
Continental drift evidence
Bed
24. 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.
Carbonate rocks
Crystal lattice
Geothermal gradient
Continental drift hypothesis
25. Soil section below the O-horizon - humus has decayed further and has mixed with mineral grains (clay - silt - and sand). Water percolating through this horizon causes chemical weathering reactions to occur and produces ions in solution and new clay m
A-horizon
Columnar jointing
Melting
Rock layering
26. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Polymorphs
Volatiles
Lapilli
Hydrolysis
27. Mineral group; olivine group - pyroxene group - amphibole group.
Clastic sedimentary rocks
Lapilli
Dark Silicates
Plates
28. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Five steps of clastic sedimentary rock formation
Symmetry
Chemical sedimentary rocks
Gem
29. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Fracture zones
Soil Horizons
atmospheres (atm)
Symmetry
30. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Magma
Ash
Crystal habit
Mafic
31. The removal of soil by running water or by wind.
Pyroclastic flows
Mafic
Streak
Soil erosion
32. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Silicate minerals
Dolostone
Granitic magma
Source rock composition
33. Outer surface level of Earth; composed of granite - basalt - and gabbro. Continental: mostly about 35-40km thick . Oceanic: about 7-10km thick. Oxygen - by far the most abundant element.
Ripples
Root wedging
Crust
Regolith
34. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Solid-state diffusion
Source rock composition
Lapilli
Fracture and cleavage
35. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Color
Felsic
Bedrock
Salt wedging
36. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
12km
Hot-spot track
Mafic
Shield volcano
37. An envelope of gas surrounding Earth consisting of 78% nitrogen (N2) and 28% oxygen (O2) - with minor amounts 1% of argon - carbon dioxide - methane - etc. And 99% of the gas in the atmosphere lies below 50km.
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38. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Biomineralization
Dolostone
Frost wedging
Area of igneous activity
39. Type of lava flow; surface layer of the lava freezes and then breaks up due to the continued movement of lava underneath - becomes a jumble of sharp - angular fragments - yielding a rubbly flow.
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40. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Glass
Gabbro
Hydrosphere
Chemical weathering
41. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Precipitation
Subduction
Grain sizes
Igneous rocks
42. A submarine suspension of sediment.
ravertine
Streak
Turbidity current
Lava tube
43. 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.
Composite cone (stratovolcano)
Explosive eruptions
Dolostone
Fracture zones
44. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Native metals
Rock texture
Igneous rocks
Arkose
45. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Erosion
Lava
Root wedging
Basalt
46. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
3.5km (2 miles)
Clastic sedimentary rocks
Five steps of clastic sedimentary rock formation
Volcanic pipes/necks
47. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Limestone
Extrusive igneous rock
Tuff
Earth's atmosphere
48. 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.
Upper mantle
Factors of magma cooling time
Deep-ocean trenches
C-horizon
49. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Assimilation
Sedimentary structure
Superplumes
Fumerolic mineralization
50. Sublayer of the mantle - depth of 660km.
Calderas
Conchoidal fractures
Upper mantle
Basalt