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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. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Regression
Weathering
Evaporites
Mineral
2. 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
Sea-floor spreading
Native metals
650-1100 degrees C
Hardness
3. 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.
Magnetic declination
Limestone
pahoehoe
Elemental composition of Earth
4. An insulated - tunnel-like conduit through which lava moves within a flow.
Streak
Sedimentary structure
Lava tube
Crust
5. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Dunes
Peridotite
Luster
Source rock composition
6. Distinguishing feature of magma; the composition of the melt reflects the composition of the solid from which it was derived. Not all magmas form from the same source rock - therefore not all magmas have the same compositions.
Biochemical sedimentary rocks
Coal
Source rock composition
Lower mantle
7. 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
Ignimbrite
Crystal
Apparent polar-wander path
Erosion
8. 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
Regression
Stoping
Bathymetry
A-horizon
9. Most common mineral on Earth; compose over 95% of the continental crust. Consist of combinations of a fundamental building block called silicon-oxygen tetrahedron - different groups: independent tetrahedra - single chains - double chains - sheet sili
Silicate minerals
Saprolite
Magnetic anomaly
Transition zone
10. 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.
Fractional crystallization
Factors of magma cooling time
Deposition
Light silicates
11. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Transform plate boundary
Oxidation
Mineral crystal destruction
Magma mixing
12. 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
Marine magnetic anomaly
Outer core
Turbidity current
13. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Physical weathering
Limestone
Transported soil
Siltstone and mudstone
14. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Sedimentary structure
Seamount chains
atmospheres (atm)
Mineral
15. 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.
Fumerolic mineralization
Assimilation
Relative plate velocity
The effect of gas pressure on eruptive style
16. The resistance to flow of magma. Reflects its distinct silica content - for silica tends to polymerize - meaning it links up to form long - chainlike molecules whose presence slows down the flowing ability of magma. Thus felsic magmas flow less easil
Magnetic inclination
Viscosity
Mafic
Silicate minerals
17. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Magnetic declination
Fissure eruptions/lava plateaus
Felsic
Native metals
18. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Chemical sedimentary rocks
Specific gravity
Volatiles
Siltstone and mudstone
19. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Plates
Dike
Organic chemicals
Asthenosphere
20. Process occurring after sediment has been compacted - can then be bounded together to make coherent sedimentary rock. Binding material consists of minerals (commonly quartz or calcite).
triple junction
Magma mixing
Cementation
Volatiles
21. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Mineral
Rock composition
Evaporites
Sill
22. Distinguishing feature of magma; the process where different magmas formed in different locations from different sources may come in contact within a magma chamber prior to freezing. Thus the originally distinct magmas mix to create a new - different
Melts
Magma mixing
Metamorphic rocks
Factors classifying clastic sedimentary rocks
23. When different rocks in an outcrop undergo weathering at different rates.
Differential weathering
Transform plate boundary
Precipitation
Shield volcano
24. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Color
Lapilli
Biochemical sedimentary rocks
Basaltic composition
25. After sand has lost its feldspar composition due to weathering over time - sediment composed entirely of quartz grains gets buried and lithified to form this type of rock.
12km
Seamount chains
Lava domes
Quartz sandstone
26. 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.
Sandstone
Large Igneous Provinces (LIPs)
Magnetic inclination
Dike
27. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Chemical weathering
Ultramafic
Graded bed
Gabbro
28. 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 -
Magma mixing
Lithification
Redbeds
Mid-ocean ridges
29. 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.
B-horizon
Glass
Regression
Strata
30. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Mid-ocean ridges
Arkose
Limestone
Granitic composition
31. An exposure of bedrock.
Grain sizes
Stratagraphic formation
Siltstone and mudstone
Outcrop
32. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Gabbro
Agrillaceous rocks
Ripples
Factors of magma cooling time
33. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Apparent polar-wander path
Caliche
Siltstone and mudstone
Subsidence
34. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
E-horizon
Chemical sedimentary rocks
Decompression
Shield volcano
35. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Graded bed
Salt wedging
Laccolith
Sulfates
36. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Source rock composition
Convective flow
Effusive eruptions
Relative plate velocity
37. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Mineral crystal destruction
Hydrosphere
Jointing
Factors classifying clastic sedimentary rocks
38. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Subsidence
Gabbro
Transform fault
Convective flow
39. 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.
Oxides
Sill
Dike
Effusive eruptions
40. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Pyroclastic flows
Continental drift evidence
Hydrolysis
Magnetic declination
41. Weathering - erosion - transportation - deposition - and lithification.
Pyroclastic flows
Area of igneous activity
Five steps of clastic sedimentary rock formation
Caliche
42. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Plates
Seamount chains
Granite
Extrusive igneous rock
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
Mineral crystal destruction
Felsic - intermediate - mafic - ultramafic
Diagenesis
Bedding
44. 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.
Zone of accumulation
Fracture and cleavage
Sulfides
Pangaea
45. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
Magnetic anomaly
pahoehoe
Abyssal plains
Symmetry
46. 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.
Continental drift hypothesis
Oxides
Cinder cone
Sedimentary Basins
47. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Gabbro
Heat transfer
Depositional environment
Silicate minerals
48. Molten rock beneath Earth's surface.
Hardness
Plutons
Magma
Relative plate velocity
49. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Metals
Strata
Lithification
Andesitic lava flows
50. The way in which the atoms are packed together within a mineral by chemical bonds. Five difference types of bonding can occur - covalent - ionic - metallic - Van der Waal's - and hydrogen.
Melting
Soil erosion
Depositional environment
Crystal structure