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Test your basic knowledge |
Geology
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Subject
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science
Instructions:
Answer 50 questions in 15 minutes.
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Match each statement with the correct term.
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1. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Fracture and cleavage
Elemental composition of Earth
Lapilli
Partial melting
2. 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
Silicate minerals
Fumerolic mineralization
C-horizon
Viscosity
3. 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
Dipole
Magnetic reversals
Sea-floor spreading
Area of igneous activity
4. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Transform plate boundary
Andesitic lava flows
Basaltic magma
Volcanic pipes/necks
5. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Pyroclastic debris
Calderas
Basaltic composition
Clastic
6. The burial and lithification of angular or rounded clasts form these types of rocks.
Dark Silicates
Streak
Conglomerate
Silicates
7. Highest soil horizon; consists almost entirely of organic matter and contains barely any mineral matter. Surface level has 'litter' and deeper it contains 'humus'. Part of the zone of leaching.
Andesitic lava flows
Rock texture
pahoehoe
O-horizon
8. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Elemental composition of Earth
C-horizon
Granitic magma
Subsidence
9. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Clastic sedimentary rocks
Sedimentary Basins
Slab-pull force
Relative plate velocity
10. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Mantle plume
Facets
Calderas
Intermediate
11. 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.
Alloy
Fractional crystallization
Grain sizes
Fracture zones
12. 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
Volatiles
Light silicates
Loam
Felsic - intermediate - mafic - ultramafic
13. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
Cross beds
Source rock composition
Earth's atmosphere
pahoehoe
14. Two different minerals which have the same composition but have different crystal structures.
Polymorphs
Crust
B-horizon
Regolith
15. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Mantle
Fragmental igneous rocks
Continental shelf
Stoping
16. Tree roots that grow into joints can push those joints open in this process.
Mafic
Root wedging
B-horizon
Tuff
17. Sedimentary rock composed of quartz.
Oxidation
Siliceous rocks
Lava tube
Mantle
18. Lava flowing on dry land cools more slowly that lava erupting underwater.
The effect of the environment on eruptive style
The effect of gas pressure on eruptive style
Fracture and cleavage
Area of igneous activity
19. Chemical weathering during Which minerals dissolve into water.
Mantle
Dissolution
Fumerolic mineralization
Five steps of clastic sedimentary rock formation
20. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Volcanic blocks/bombs
Plutons
Stoping
Abyssal plains
21. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Special properties of minerals
Felsic
Sulfates
Apparent polar-wander path
22. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Bathymetry
Outcrop
Sea-floor spreading
Superplumes
23. A fine spray of lava instantly freezes to form fine particles of glass.
Ash
Lower mantle
Ultramafic
Transported soil
24. 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.
Zone of accumulation
Regolith
Transition zone
Rock texture
25. The crust moves away from the Mid-Atlantic Ridge axis at a rate of 1cm per year. This velocity of sea-floor spreading is determined by the relationship between the paleomagnetic anomaly-stripe's width and the reverse polarity duration - the data reve
Biomineralization
Spreading rate
Regression
rifting
26. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Relative plate velocity
Limestone
Pyroclastic debris
Crystalline
27. 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
Graded bed
Crystalline
Grain sizes
28. 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.
Plutons
Large Igneous Provinces (LIPs)
Soil
Mineral crystal destruction
29. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Large Igneous Provinces (LIPs)
Continental drift hypothesis
Lithosphere
Arkose
30. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Dolostone
Lava tube
Phreatomagmatic eruptions
Native metals
31. Form when solid materials become hot and transform into liquid - example - molten rock.
Color
Melts
Magnetic inclination
Erosion
32. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Physical weathering
Stratagraphic formation
Peridotite
rifting
33. When different rocks in an outcrop undergo weathering at different rates.
Differential weathering
Abyssal plains
Regolith
Explosive eruptions
34. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Magma mixing
Depositional environment
Magma
Mantle
35. A plate boundary at which one plate slips along the side of another plate. No new plate is formed and no old plate is consumed. But the grinding between the plates generates frequent and destructive earthquakes.
Siltstone and mudstone
The effect of gas pressure on eruptive style
C-horizon
Transform plate boundary
36. A place where three plate boundaries intersect at a point.
Metamorphic rocks
triple junction
Luster
Partial melting
37. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Continental drift evidence
Factors of magma cooling time
Tephra
Seamount chains
38. 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.
Heat transfer
Fragmental igneous rocks
Streak
Spreading rate
39. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Sill
Facets
Physical weathering
Convective flow
40. 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
Clastic sedimentary rocks
Salt wedging
Stratagraphic formation
41. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Granitic composition
Depositional environment
Euhedral crystal
Limestone
42. An exposure of bedrock.
Upper mantle
Outcrop
Earth's atmosphere
Mid-ocean ridges
43. 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
Symmetry
Silicate minerals
Crust
A-horizon
44. 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.
Viscosity
Hot spots
Oxidation
Pyroclastic debris
45. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Arkose
Siliceous rocks
Siltstone and mudstone
Regolith
46. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Stratagraphic formation
Mineral
Tuff
Reason for Earth's internal heat
47. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Elemental composition of Earth
Continental shelf
Chemical weathering
Hydration
48. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Divergent plate boundary
Heat transfer
Saprolite
Frost wedging
49. A mineral's growth that is uninhibited - has well-formed crystal faces.
Rock texture
Magma mixing
Magnetic anomaly
Euhedral crystal
50. 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
Mineral
Mafic
Dunes
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