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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 type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Chemical weathering
Chemical sedimentary rocks
Seamount chains
Limestone
2. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Gabbro
Specific gravity
Andesitic lava flows
The effect of the environment on eruptive style
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 -
Special properties of minerals
rifting
Paleomagnetism
Limestone
4. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Turbidite
Calderas
Thermal expansion
O-horizon
5. 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.
Subduction
Stoping
Stratagraphic formation
Bathymetry
6. 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.
Metamorphic foliation
Gem
Rock texture
Relative plate velocity
7. Deeper sublayer of the mantle - depth of 660km to 2900km.
Soil
Tephra
Lower mantle
Luster
8. Rock formations still attached to the Earth's crust.
Bedrock
triple junction
Coal
Rock-forming silicate minerals
9. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Coal
Volatiles
Agrillaceous rocks
Volcano
10. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Transform fault
Extrusive igneous rock
Hydrolysis
Bedding
11. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Tephra
O-horizon
Fracture zones
Dike
12. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Arkose
Crystal lattice
atmospheres (atm)
Subduction
13. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Topography
Cross beds
Conchoidal fractures
Thermal expansion
14. Sedimentary rocks made up of the shells of organisms.
Pangaea
Volatiles
Large Igneous Provinces (LIPs)
Biochemical sedimentary rocks
15. 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
Fumerolic mineralization
Tuff
Subduction
Why magma rises
16. Carbon-containing compounds that either occur in living organisms - or have characteristics that resemble the molecules within living organisms. Examples - oil - protein - plastic - fat - and rubber.
Salt wedging
Diagenesis
Organic chemicals
Arkose
17. 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.
Bathymetry
650-1100 degrees C
Upper mantle
Crystal structure
18. An exposure of bedrock.
atmospheres (atm)
Dark Silicates
Outcrop
Strata
19. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Weathering
Thermal expansion
Effusive eruptions
Felsic
20. 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.
Asthenosphere
3.5km (2 miles)
triple junction
Paleomagnetism
21. Along much of the perimeter of the Pacific Ocean - the ocean floor reaches astounding depths of 8-12km. These areas define elongate troughs - and they border volcanic arcs - the curving chains of active volcanoes.
triple junction
Deep-ocean trenches
Redbeds
Divergent plate boundary
22. A plate boundary at which two plates move apart from one another by process of sea-floor spreading. Mid-ocean ridges or simply a ridge. New crust is formed at ridges through the buoyant rising of magma from beneath the surface and solidifies to creat
Divergent plate boundary
Relative plate velocity
Inner core
The effect of gas pressure on eruptive style
23. Type of magma; low in silica - fluid - crystallize at high temperatures.
Divergent plate boundary
Basaltic magma
Soil Horizons
Batholiths
24. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Lapilli
Plutons
Marine magnetic anomaly
Mineral
25. 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.
Crystalline igneous rocks
Transported soil
Depositional environment
Asthenosphere
26. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Mafic
Metals
Mid-ocean ridges
atmospheres (atm)
27. Consists of rock and sediment that has been modified by physical and chemical interaction with organic material and rainwater - over time - to produce a substrate that can support the growth of plants.
Batholiths
Volcanic blocks/bombs
Soil
Bed
28. 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
Cross beds
Siliceous rocks
Sedimentary Basins
29. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Redbeds
Agrillaceous rocks
Divergent plate boundary
Gem
30. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Outer core
a'a'
Transgression
Redbeds
31. Sedimentary rock composed of calcite or dolomite.
Quartz sandstone
Carbonate rocks
Divergent plate boundary
Plate tectonics
32. Process that occurs after the sediment has been buried - pressure cause by the overburden squeezes out water and air that had been trapped between clasts - and the clasts press together tightly.
Quartz sandstone
A-horizon
Compaction
Sedimentary rocks
33. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Basaltic composition
Luster
Magma
Crystal lattice
34. 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.
Melts
Fumerolic mineralization
Siltstone and mudstone
Glass
35. Sublayer of the mantle - depth of 660km.
Outer core
Lava tube
Upper mantle
Redbeds
36. 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.
Mid-ocean ridges
Continental rift
Conchoidal fractures
Soil Horizons
37. Type of volcanic eruption; takes place when water gains access to the hot rock around the magma chamber and suddenly transforms into steam - a pyroclastic eruption involving the reaction of water with magma.
Magma mixing
Phreatomagmatic eruptions
Effusive eruptions
Earth's atmosphere
38. Physical property of a mineral; refers to the color of a powder produced by pulverizing the mineral. Provides a fairly reliable clue to the mineral's identity - since the color of the mineral powder tends to be less variable than the color of the who
Dike
Chemical weathering
Graded bed
Streak
39. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Regolith
Crystal habit
Felsic
Dunes
40. 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
The core
Melting
Crystal
41. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Crust
Volcano
Chert
Euhedral crystal
42. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
3.5km (2 miles)
Tuff
Magma
Plates
43. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Viscosity
Volcanic blocks/bombs
Salt wedging
Oxidation
44. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Lithification
Intermediate
Spreading rate
Magnetic anomaly
45. The nature of Earth's magnetic field - like the familiar magnetic field around a bar magnet - has a North and South pole. The magnetic field is drawn with field lines - the paths along Which magnets would align - or charged particles would flow - if
Siliceous rocks
Hydration
Sulfates
Dipole
46. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Xenolith
Why magma rises
atmospheres (atm)
Alloy
47. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Volcano
Crystalline igneous rocks
Basaltic magma
Convergent plate boundary
48. Sedimentary rock composed of quartz.
Rock-forming silicate minerals
Volatiles
Siliceous rocks
Luster
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
Apparent polar-wander path
Deposition
Facets
Ridge-push force
50. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Arkose
Rock-forming silicate minerals
Gabbro
Oxides