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Test your basic knowledge |
Geology
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Study First
Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
If you are not ready to take this test, you can
study here
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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. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Xenolith
Reason for Earth's internal heat
Crystalline
Erosion
2. 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.
Divergent plate boundary
Andesitic lava flows
Continental drift evidence
Fumerolic mineralization
3. 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 -
Basaltic lava flows
Mantle plume
Special properties of minerals
Seamount chains
4. 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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5. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Special properties of minerals
Fissure eruptions/lava plateaus
Volcano
Coal
6. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Magma mixing
Limestone
Subduction
Transported soil
7. 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.
Spreading rate
Bed
Dark Silicates
Continental drift hypothesis
8. Lava flowing on dry land cools more slowly that lava erupting underwater.
Grain sizes
Convergent plate boundary
Solid-state diffusion
The effect of the environment on eruptive style
9. A type of soil consisting of about 10-30% clay and the rest silt and sand. Pores remain between grains so that water and air can pass through and roots can easily penetrate.
Loam
The effect of viscosity on eruptive style
Fracture and cleavage
Dipole
10. Type of soil; forms directly from underlying bedrock.
Carbonate rocks
Bed
Tephra
Residual soil
11. Layer that lies below the lithosphere - and is the portion of the mantle in which rock can flow (slowly; 10-15cm per year) despite still being solid. Entirely within the mantle and lies below a depth of 100-150km.
Chemical weathering
Siltstone and mudstone
Asthenosphere
Mantle
12. The display of the pattern of atoms or ions within a mineral. Meaning that the shape of one part of a mineral is a mirror image of the shape of another part.
Area of igneous activity
Sea-floor spreading
Symmetry
Arkose
13. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Sandstone
Arkose
Lower mantle
Native metals
14. 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
Metamorphic foliation
collision
triple junction
Why magma rises
15. 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
The effect of gas pressure on eruptive style
Continental rift
Intermediate
Magnetic anomaly
16. 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.
Subsidence
Dike
Crystal habit
Fracture zones
17. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Metamorphic foliation
Intrusive igneous rock
Factors classifying clastic sedimentary rocks
Gem
18. The process by which sediment settles out of the transporting medium.
Rock composition
Ripples
Silicate minerals
Deposition
19. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Outcrop
Laccolith
C-horizon
Deep-ocean trenches
20. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Pyroclastic flows
Hardness
Felsic - intermediate - mafic - ultramafic
Root wedging
21. The freely pivoting up and down compass needle's angle of tilt relative to the location upon the Earth's surface. At the equator - the specialized magnetic needle would position horizontally and at a magnetic pole it would point straight down.
Magnetic inclination
Andesitic lava flows
The effect of viscosity on eruptive style
Volatiles
22. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Basaltic magma
The core
Dunes
Graded bed
23. 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.
Sedimentary structure
Hot spots
Loam
Metamorphic foliation
24. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Pyroclastic flows
Hot spots
Metamorphic foliation
Volcanic pipes/necks
25. Two different minerals which have the same composition but have different crystal structures.
Apparent polar-wander path
Carbonate rocks
Composite cone (stratovolcano)
Polymorphs
26. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Five steps of clastic sedimentary rock formation
Felsic - intermediate - mafic - ultramafic
Mafic
Hardness
27. A process occurring when sea level falls - the coast migrates seaward.
Regression
Large Igneous Provinces (LIPs)
E-horizon
Lower mantle
28. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Turbidite
The effect of viscosity on eruptive style
Transform plate boundary
Mantle
29. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Fracture and cleavage
atmospheres (atm)
Zone of accumulation
Special properties of minerals
30. 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.
Dissolution
Paleomagnetism
Explosive eruptions
Granitic magma
31. 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
Silicate minerals
Columnar jointing
Salt wedging
Sedimentary structure
32. A fine spray of lava instantly freezes to form fine particles of glass.
Pangaea
Silicate minerals
Ash
Rock layering
33. 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.
Columnar jointing
Polymorphs
Rock composition
Shield volcano
34. Molten rock beneath Earth's surface.
Magma
Andesitic lava flows
Granitic magma
Deep-ocean trenches
35. 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.
Fracture zones
Rock-forming silicate minerals
Residual soil
Hydration
36. Physical property of a mineral; refers to the shape (morphology) of a single crystal with well-formed crystal faces - or to the character of an aggregate of many well-formed crystals that grew together as a group. Depends on the internal arrangement
Crystal habit
Melting
Silicates
Pyroclastic debris
37. 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.
Magma mixing
Chert
Metamorphic rocks
Metamorphic foliation
38. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Why magma rises
Light silicates
Slab-pull force
Continental shelf
39. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Physical weathering
Peridotite
Dissolution
Silicate minerals
40. 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
E-horizon
Volatiles
Why magma rises
Compaction
41. Sedimentary rock composed of calcite or dolomite.
Chemical weathering
Weathering
Carbonate rocks
Lava
42. 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
Crystalline igneous rocks
Root wedging
Relative plate velocity
43. 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 -
Lapilli
Mid-ocean ridges
Saprolite
Rock-forming silicate minerals
44. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Sedimentary structure
Turbidity current
Organic chemicals
Lithosphere
45. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Hot-spot track
Soil erosion
Biomineralization
Basaltic lava flows
46. The removal of soil by running water or by wind.
Fractional crystallization
Zone of leaching
Residual soil
Soil erosion
47. A term used for all the physical - chemical - and biological processes that transform sediment into sedimentary rock and that alter characteristics of sedimentary rock one the rock has formed.
Light silicates
Crystal
Diagenesis
Chert
48. 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
Plate tectonics
Carbonates
Sulfates
Outer core
49. Develops because mid-ocean ridges lie at a higher elevation than the adjacent abyssal plains of the ocean. The surface of the sea floor overall slopes away from the ridge axis. Gravity causes the elevated lithosphere at the ridge axis to push on the
Metamorphic foliation
Streak
Volatiles
Ridge-push force
50. A mineral's growth that is uninhibited - has well-formed crystal faces.
Volcano
Five steps of clastic sedimentary rock formation
Euhedral crystal
Conchoidal fractures