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Test your basic knowledge |
Geology
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Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
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Match each statement with the correct term.
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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 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
Shield volcano
Dissolution
Transform plate boundary
2. 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
Diagenesis
Magnetic anomaly
The effect of gas pressure on eruptive style
The effect of the environment on eruptive style
3. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Volcano
Plutons
12km
Transported soil
4. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
ravertine
Clastic
Symmetry
Viscosity
5. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Mid-ocean ridges
Seamount chains
Glass
Dipole
6. Sedimentary rock composed of clay.
Silicate minerals
Transported soil
Agrillaceous rocks
Hydration
7. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Crystal habit
Magma mixing
triple junction
Paleopole
8. The process by which sediment settles out of the transporting medium.
Deposition
Apparent polar-wander path
Felsic
Agrillaceous rocks
9. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
12km
Transported soil
Coal
Paleopole
10. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Hot spots
Lapilli
Magma
Crystal habit
11. By melting - dissolving - or other chemical reactions.
Basalt
Decompression
Outer core
Mineral crystal destruction
12. Mineral class; consist of a metal cation bonded to a sulfide anion. Examples - galena and pyrite. Many have a metallic luster. Can also be considered ores with high proportions of metal within the mineral.
Soil
atmospheres (atm)
Solid-state diffusion
Sulfides
13. Layering in sedimentary rocks.
Lithosphere
Bedding
Agrillaceous rocks
Sedimentary structure
14. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
A-horizon
Depositional environment
Native metals
Saprolite
15. The most important mineral group; comprise the most rock-forming minerals - they are very abundant due to large % of silicon and oxygen in Earth's crust. Examples - oxygen - silica - aluminum.
Silicates
Weathering
Rock-forming silicate minerals
Regolith
16. 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
Symmetry
A-horizon
Volcanic blocks/bombs
Convergent plate boundary
17. Rocks which develop when hot molten rock cools and freezes solid.
Granitic magma
Igneous rocks
Streak
12km
18. 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.
Siliceous rocks
Crystal structure
Basaltic magma
Transported soil
19. 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
Redbeds
Mineral
atmospheres (atm)
Decompression
20. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Intrusive igneous rock
Convergent plate boundary
Apparent polar-wander path
Chemical sedimentary rocks
21. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Melts
Salt wedging
Depositional environment
Redbeds
22. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
a'a'
The effect of the environment on eruptive style
Dunes
Biomineralization
23. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Andesitic lava flows
Fractional crystallization
Igneous rocks
Columnar jointing
24. 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
Biochemical sedimentary rocks
Granitic magma
Magnetic reversals
Chert
25. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Clastic
Silicate minerals
Felsic
Mid-ocean ridges
26. Molten rock that has flowed out onto Earth's surface.
Outer core
Lava
Glassy igneous rocks
Plutons
27. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Shield volcano
Sedimentary structure
Chert
Magnetic inclination
28. 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.
Mineral crystal destruction
Transported soil
Explosive eruptions
Solid-state diffusion
29. 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
Basalt
Magnetic anomaly
Plate tectonics
Convergent plate boundary
30. 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.
Batholiths
Color
Sulfates
Crystal
31. Rock formations still attached to the Earth's crust.
Hot spots
Bedrock
Ultramafic
Mineral crystal destruction
32. Physical features of the land surface represented by changes in elevation.
12km
Hydrolysis
Cement
Topography
33. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Paleopole
Granitic composition
Chert
Magma's speed of flow
34. Process that occurs after the sediment has been buried - pressure cause by the overburden squeezes out water and air that had been trapped between clasts - and the clasts press together tightly.
Color
Compaction
Dolostone
Fracture and cleavage
35. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Phreatomagmatic eruptions
Luster
Transgression
Cementation
36. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Luster
Bed
Basalt
Sulfides
37. 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.
Outer core
Apparent polar-wander path
Superplumes
Asthenosphere
38. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Andesitic lava flows
Magma mixing
Lapilli
Evaporites
39. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Magnetic declination
Dissolution
Plutons
Transported soil
40. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Ignimbrite
Precipitation
Tephra
Factors classifying clastic sedimentary rocks
41. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Factors classifying clastic sedimentary rocks
Coal
triple junction
Regression
42. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Cement
Specific gravity
Abyssal plains
Basaltic composition
43. The intrusion of numerous plutons in a region - produces a vast composite body that may be several hundred kilometers long and over 100km wide; an immense body of igneous rock.
Glass
Batholiths
Sea-floor spreading
Crystal structure
44. 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.
Plates
Pangaea
Bedding
Crystal lattice
45. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Flood basalts
Depositional environment
Laccolith
Soil erosion
46. 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.
Diagenesis
Phreatomagmatic eruptions
Silicate minerals
Cement
47. The removal of soil by running water or by wind.
Silicates
Fractional crystallization
Soil Horizons
Soil erosion
48. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Continental drift evidence
Arkose
Magnetic anomaly
Asthenosphere
49. Two different minerals which have the same composition but have different crystal structures.
Tephra
Superplumes
Hot spots
Polymorphs
50. 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.
Sulfides
Crust
Hydrosphere
Rocks
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