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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. 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
Slab-pull force
Soil erosion
Heat transfer
2. 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.
Laterite
ravertine
Sedimentary structure
Metals
3. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Laccolith
Ignimbrite
Intermediate
Color
4. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Rhyolitic lava flows
Ash
Ignimbrite
Volcanic pipes/necks
5. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Elemental composition of Earth
Viscosity
Siliceous rocks
Conchoidal fractures
6. 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
Siliceous rocks
Caliche
Luster
7. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Lava
Chemical weathering
Soil Horizons
Oxides
8. 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
Outer core
Magnetic reversals
Light silicates
Melting
9. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
The core
Jointing
Continental drift evidence
Calderas
10. The angle between the direction that a compass needle points at a given location and the direction of the 'true' (geographic) north. Through this process - the magnetic poles never stray more than 15 degrees of latitude from the geographic pole.
Volcanic blocks/bombs
Basaltic lava flows
Magnetic declination
Granitic magma
11. 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.
Caliche
Volcanic blocks/bombs
Color
Crystal habit
12. The burial and lithification of angular or rounded clasts form these types of rocks.
Andesitic lava flows
Strata
Conglomerate
Upper mantle
13. Two different minerals which have the same composition but have different crystal structures.
Carbonates
650-1100 degrees C
Polymorphs
Hot spots
14. 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.
Root wedging
Shield volcano
Cinder cone
Diagenesis
15. A rock made of solid mass of glass - or of tiny crystals surrounded by glass. Reflect light as glass does and tend to break conchoidally. Examples - obsidian - tachylite - pumice.
Halides
Glassy igneous rocks
Crystal lattice
Deposition
16. Layering in sedimentary rocks.
Intermediate
Bedding
Flood basalts
Cement
17. 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.
Fissure eruptions/lava plateaus
Slab-pull force
Biochemical sedimentary rocks
Asthenosphere
18. Rocks whose crystals interlock with each other.
Divergent plate boundary
Crystalline
Abyssal plains
Compaction
19. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Lava
12km
Shield volcano
Ash
20. Physical features of the land surface represented by changes in elevation.
Crust
Intrusive igneous rock
Topography
Continental drift evidence
21. The removal of soil by running water or by wind.
Batholiths
Volcanic pipes/necks
The core
Soil erosion
22. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Relative plate velocity
Tephra
Native metals
Dolostone
23. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Conchoidal fractures
Caliche
Depositional environment
Dunes
24. 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.
Partial melting
Paleomagnetism
Asthenosphere
Crust
25. Mineral class; consist of metal cations bonded by oxygen anions. Examples - hematite and magnetite. Some contain a relatively high proportion of metal atoms - and thus are ore minerals.
Stratagraphic formation
Oxides
Solid-state diffusion
Geothermal gradient
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
Jointing
Apparent polar-wander path
Transgression
Felsic - intermediate - mafic - ultramafic
27. Deeper sublayer of the mantle - depth of 660km to 2900km.
Effusive eruptions
Metamorphic rocks
Siltstone and mudstone
Lower mantle
28. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Magma's speed of flow
Siltstone and mudstone
Superplumes
Hydrolysis
29. A process occurring when sea level falls - the coast migrates seaward.
Magma
Regression
Mantle
Dolostone
30. Breaks intact rocks into unconnected grains or chunks - collectively called debris or detritus. Grain size from largest to smallest: boulders - cobbles - pebbles - sand - silt - mud/clay.
Subduction
Physical weathering
Carbonates
Continental drift evidence
31. The speed of the movements of the plates with respect to the speed of the other plates' movements. Absolute plate velocity is a measure of the movement of any plates relative to a fixed point in the mantle.
Relative plate velocity
Sill
Transform fault
The effect of gas pressure on eruptive style
32. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Gabbro
Bedrock
Lava domes
C-horizon
33. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Hydrolysis
Mantle plume
Glassy igneous rocks
Magnetic anomaly
34. The bottom portion of the upper mantle - the interval lying between 400km and 660km deep. Here within the Earth - the character of the mantle undergoes a series of abrupt changes.
Transition zone
Extrusive igneous rock
Soil erosion
Bathymetry
35. The shape of the sea floor surface. Investigation of the sea-floor revealed the presence of several important features: mid-ocean ridges - deep-ocean trenches - seamount chains - and fracture zones.
Bathymetry
Caliche
Relative plate velocity
Turbidity current
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.
Ridge-push force
Basaltic composition
Zone of accumulation
E-horizon
37. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Subduction
Marine magnetic anomaly
Felsic
Volcanic blocks/bombs
38. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Igneous rocks
Ash
Specific gravity
39. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Geothermal gradient
Superplumes
Magnetic anomaly
ravertine
40. Physical property of a mineral; represents the density of a mineral - as specified by the ratio between the weight of a volume of the mineral and the weight of an equal volume of water a 4 degrees C.
Hydrolysis
Specific gravity
Partial melting
Biochemical sedimentary rocks
41. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Pyroclastic debris
Frost wedging
Ultramafic
Metamorphic foliation
42. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Bed
Grain sizes
Magnetic anomaly
Mineral crystal destruction
43. 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
Glass
Outer core
Turbidite
Sulfates
44. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Earth's atmosphere
Lithosphere
Granitic composition
Caliche
45. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Quartz sandstone
Fracture zones
Coal
Plates
46. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Siliceous rocks
ravertine
Conchoidal fractures
Mid-ocean ridges
47. Fluid basaltic lava extruded from crustal fractures called fissures.
Outer core
Solid-state diffusion
Biochemical sedimentary rocks
Fissure eruptions/lava plateaus
48. Form when solid materials become hot and transform into liquid - example - molten rock.
Sedimentary structure
Siltstone and mudstone
Melts
Lava tube
49. 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.
Arkose
Factors of magma cooling time
Partial melting
Stratagraphic formation
50. 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.
Phreatomagmatic eruptions
Transform fault
Topography
Volatiles