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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. An exposure of bedrock.
Outcrop
Euhedral crystal
Dike
Hydrolysis
2. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Depositional environment
Silicates
Outer core
Laccolith
3. 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
Hardness
Magnetic anomaly
Zone of accumulation
The effect of viscosity on eruptive style
4. Type of soil; forms directly from underlying bedrock.
Residual soil
Magma's speed of flow
Magnetic declination
Thermal expansion
5. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Magnetic inclination
Dolostone
650-1100 degrees C
Magma
6. Two different minerals which have the same composition but have different crystal structures.
Magnetic declination
Hot spots
Mid-ocean ridges
Polymorphs
7. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Explosive eruptions
Oxidation
Basaltic lava flows
Heat transfer
8. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Turbidite
Diagenesis
Euhedral crystal
Plutons
9. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Intermediate
The effect of the environment on eruptive style
Apparent polar-wander path
Lava domes
10. Sedimentary rocks made up of the shells of organisms.
Rock layering
Cement
Rock-forming silicate minerals
Biochemical sedimentary rocks
11. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Magma's speed of flow
Gem
Hot-spot track
Color
12. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Rhyolitic lava flows
Loam
Tuff
Transform plate boundary
13. Molten rock that has flowed out onto Earth's surface.
Lava
Laccolith
Solid-state diffusion
Fracture zones
14. 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
Continental drift hypothesis
A-horizon
Siltstone and mudstone
Siliceous rocks
15. 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
Soil
Loam
Magma mixing
Deposition
16. 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
Hot-spot track
Cement
Silicate minerals
Metals
17. 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.
Pangaea
Transform fault
Glassy igneous rocks
Decompression
18. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Dark Silicates
Assimilation
Andesitic lava flows
Siltstone and mudstone
19. An insulated - tunnel-like conduit through which lava moves within a flow.
Frost wedging
Ash
Basaltic lava flows
Lava tube
20. The supercontinent; existence proposed by Wegener - suggested that the supercontinent later fragmented into separate continents that then drifted apart - moving slowly to their present positions.
Pangaea
Large Igneous Provinces (LIPs)
Flood basalts
Compaction
21. 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
3.5km (2 miles)
Viscosity
Volatiles
22. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Tephra
3.5km (2 miles)
Apparent polar-wander path
Sandstone
23. Places with particularly voluminous quantities of magma erupting or intruding.
Factors classifying clastic sedimentary rocks
Symmetry
Topography
Large Igneous Provinces (LIPs)
24. 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
Calderas
Subduction
Magma mixing
Mineral
25. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Crystal lattice
Abyssal plains
Diagenesis
Pangaea
26. Contributes to formation of soil; occurs when rainwater percolates through the debris and carries dissolved ions and clay flakes downward - This is the region where the downward transport occurs.
Zone of leaching
Metamorphic rocks
Sedimentary structure
C-horizon
27. 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.
Precipitation
Bedding
Silicates
Color
28. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Ripples
Silicates
Magma mixing
Regolith
29. Mineral class; the fundamental component within these types of minerals in the Earth's crust is the silicon-oxygen tetrahedron anionic group - a silicon atom surrounded by four oxygen atoms that are arranged to define the corners of a tetrahedron - a
Compaction
Silicates
Thermal expansion
Hydration
30. 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.
Transform fault
Weathering
Marine magnetic anomaly
Soil
31. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Andesitic lava flows
Batholiths
Thermal expansion
Mafic
32. 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.
Reason for Earth's internal heat
Hot spots
Glassy igneous rocks
Crystal structure
33. Fluid basaltic lava extruded from crustal fractures called fissures.
Fissure eruptions/lava plateaus
Turbidity current
Volatiles
Sulfates
34. Mineral class; consist of a metal cation bonded to the anionic group. Many form by precipitation out of water at or near the Earth's surface. Example - gypsum.
Marine magnetic anomaly
Continental rift
Sulfates
Silicate minerals
35. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Plates
Compaction
Hydration
Thermal expansion
36. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
C-horizon
Why magma rises
A-horizon
Peridotite
37. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Evaporites
Siliceous rocks
Limestone
Factors classifying clastic sedimentary rocks
38. Theory confirmed by 1968 - geologists had developed the complete model of continental drift - sea-floor spreading - and subduction. Within this model - Earth's lithosphere consists of about 20 distinct pieces - or plates - that move relative to each
Extrusive igneous rock
Paleomagnetism
Plate tectonics
Melting
39. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Mantle
Biomineralization
Convergent plate boundary
The effect of the environment on eruptive style
40. A fine spray of lava instantly freezes to form fine particles of glass.
Gem
Ash
Mid-ocean ridges
Lava tube
41. 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
Source rock composition
Sulfates
Mantle plume
42. Sedimentary rock composed of clay.
Evaporites
Agrillaceous rocks
Sea-floor spreading
Sulfates
43. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Magma
Sedimentary rocks
Redbeds
Decompression
44. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
Plutons
Seamount chains
3.5km (2 miles)
Siltstone and mudstone
45. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Pyroclastic flows
The effect of viscosity on eruptive style
Hydration
Factors of magma cooling time
46. Distinguishing feature of magma; the process where magma sits in a magma chamber before completely solidifying - it may incorporate chemicals derived from the walls rocks of the chamber.
Agrillaceous rocks
Residual soil
A-horizon
Assimilation
47. Core division; from a depth of 5155km down to Earth's center at 6371km. A radius of about 1220km - is solid iron-nickel alloy - can reach temperature of 4700 degrees C. Solid in nature because of subjection to greater pressure - keeps atoms from wand
Magma mixing
Xenolith
Root wedging
Inner core
48. The removal of soil by running water or by wind.
Geothermal gradient
Soil erosion
Five steps of clastic sedimentary rock formation
Area of igneous activity
49. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Continental shelf
Marine magnetic anomaly
Crust
Explosive eruptions
50. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Fractional crystallization
Mineral
Source rock composition
Assimilation