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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. Sedimentary rock composed of quartz.
Composite cone (stratovolcano)
Siliceous rocks
Dissolution
Color
2. 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
The effect of the environment on eruptive style
Crystal habit
Luster
Lava tube
3. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Peridotite
Transgression
ravertine
Organic chemicals
4. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Carbonates
Inner core
Lava tube
Strata
5. The difference between the expected strength of the Earth's main field at a certain location and the actual measure strength of the magnetic field at that location. Places where the field strength is stronger that expected are positive anomalies - an
The effect of the environment on eruptive style
Metals
Magnetic anomaly
Convergent plate boundary
6. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Plate tectonics
Dissolution
Volcanic blocks/bombs
Hydrolysis
7. 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.
Transition zone
Hardness
Relative plate velocity
Explosive eruptions
8. 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.
Composite cone (stratovolcano)
Lithification
Conglomerate
Symmetry
9. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Coal
Lava tube
Sulfates
The core
10. Layering in metamorphic rocks.
Metamorphic foliation
Metals
Chemical sedimentary rocks
Outcrop
11. 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 -
Clastic
Lower mantle
Mid-ocean ridges
Limestone
12. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Rock composition
Granitic magma
Jointing
Polymorphs
13. 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.
Magnetic reversals
Loam
Volatiles
3.5km (2 miles)
14. Sedimentary rocks consisting of carbon-rich relicts of plants.
Volcano
Sea-floor spreading
Saprolite
Organic sedimentary rocks
15. Rocks with a fragmental texture consist of igneous fragments that are packed together - welded together - or cemented together after having solidified. Examples - pyroclastic rocks such as tuff or breccia.
Conglomerate
Fragmental igneous rocks
Chemical weathering
Bedding
16. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Hydrolysis
Basaltic lava flows
Rock layering
Five steps of clastic sedimentary rock formation
17. By melting - dissolving - or other chemical reactions.
Mineral crystal destruction
Continental shelf
Laccolith
Hot spots
18. 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.
Sedimentary rocks
Rocks
Tuff
Ridge-push force
19. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Regression
Deep-ocean trenches
Pyroclastic debris
Hot-spot track
20. A mineral's growth that is uninhibited - has well-formed crystal faces.
Why magma rises
Shield volcano
Euhedral crystal
Fragmental igneous rocks
21. The burial and lithification of angular or rounded clasts form these types of rocks.
Outcrop
Stoping
Conglomerate
Bed
22. 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
Euhedral crystal
Inner core
Outer core
23. 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.
Metamorphic rocks
Precipitation
Pyroclastic flows
Shield volcano
24. 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.
Differential weathering
Fumerolic mineralization
a'a'
Igneous rocks
25. The combination of processes that separate rock or regolith from its substrate and carry it away. Involves abrasion - plucking - scouring - and dissolution - and is caused by air - water or ice.
Erosion
Transgression
Stoping
Lapilli
26. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Crystal habit
Jointing
Regression
Mineral
27. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Transgression
Gabbro
Euhedral crystal
Rhyolitic lava flows
28. 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.
Convergent plate boundary
Soil Horizons
Crust
Xenolith
29. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Mineral
Melting
Mafic
Fragmental igneous rocks
30. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Mineral crystal destruction
Siliceous rocks
Metals
Felsic
31. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Caliche
Transgression
Jointing
Ripples
32. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Redbeds
Metamorphic rocks
Sulfates
Convergent plate boundary
33. A plate boundary at which two plates move toward one another so that one plate sinks beneath the other. Subduction zones; Engage the sinking process known as subduction - between plates - consuming old oceanic lithosphere due to high density. Can sim
a'a'
Convergent plate boundary
Lava domes
Solid-state diffusion
34. Farther down from a zone of leaching - new mineral crystals precipitate directly out of the water or form when the water reacts with debris - this the region where the new minerals and clay collect.
The effect of viscosity on eruptive style
Zone of accumulation
Root wedging
Grain sizes
35. 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
Viscosity
Residual soil
Apparent polar-wander path
Glass
36. 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
Hot spots
Magma
Luster
37. A process occurring when sea level falls - the coast migrates seaward.
Fracture zones
Precipitation
Regression
Topography
38. Rock formations still attached to the Earth's crust.
Convective flow
Cementation
Bedrock
Heat transfer
39. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Transform plate boundary
Plutons
Laccolith
Heat transfer
40. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Chemical weathering
Pangaea
Grain sizes
Crystal habit
41. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Transform fault
Residual soil
Lithosphere
Stratagraphic formation
42. Layering in sedimentary rocks.
Peridotite
Bedding
Special properties of minerals
Pangaea
43. 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
Lapilli
Felsic - intermediate - mafic - ultramafic
Salt wedging
Basaltic magma
44. 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).
Limestone
Factors of magma cooling time
Hot spots
Silicate minerals
45. 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.
Magnetic anomaly
Native metals
Halides
Color
46. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Lava domes
Euhedral crystal
Depositional environment
Strata
47. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Tuff
Diagenesis
Magma
3.5km (2 miles)
48. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Carbonate rocks
Precipitation
Xenolith
Ultramafic
49. 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.
Sedimentary rocks
Marine magnetic anomaly
Glass
12km
50. Two different minerals which have the same composition but have different crystal structures.
Transgression
Polymorphs
Peridotite
Lithosphere