SUBJECTS
|
BROWSE
|
CAREER CENTER
|
POPULAR
|
JOIN
|
LOGIN
Business Skills
|
Soft Skills
|
Basic Literacy
|
Certifications
About
|
Help
|
Privacy
|
Terms
|
Email
Search
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. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Mantle
Volatiles
Outer core
Special properties of minerals
2. Refers to the proportions of different chemicals making up the rock - and thus the proportion chemicals affects the proportions of different minerals constituting the rock.
Rock composition
Lithosphere
Strata
Plates
3. 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.
Glass
Effusive eruptions
triple junction
Transform plate boundary
4. 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).
Sea-floor spreading
Symmetry
Cementation
Sedimentary Basins
5. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Convective flow
Granitic composition
Oxidation
Turbidite
6. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Cross beds
Xenolith
Hot-spot track
Tuff
7. 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.
Apparent polar-wander path
collision
Rock-forming silicate minerals
Crystal
8. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Regolith
Subsidence
Clastic sedimentary rocks
Solid-state diffusion
9. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Sedimentary structure
Ignimbrite
Convective flow
Seamount chains
10. 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.
Metamorphic rocks
Source rock composition
Cinder cone
Special properties of minerals
11. The burial and lithification of angular or rounded clasts form these types of rocks.
Conglomerate
Cross beds
Continental drift evidence
Granitic composition
12. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Light silicates
Intermediate
Ignimbrite
a'a'
13. 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.
Crystal lattice
Geothermal gradient
Bathymetry
Magnetic declination
14. 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.
Biomineralization
Magma
Phreatomagmatic eruptions
Soil
15. Rocks whose crystals interlock with each other.
Ripples
Diagenesis
Crystalline
Mantle
16. 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.
Lava tube
Frost wedging
Pangaea
Conglomerate
17. 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.
Quartz sandstone
triple junction
Hot spots
Solid-state diffusion
18. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Turbidite
Zone of leaching
Convective flow
Crystal habit
19. 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.
Silicate minerals
pahoehoe
Oxides
Clastic sedimentary rocks
20. Develops because mid-ocean ridges lie at a higher elevation than the adjacent abyssal plains of the ocean. The surface of the sea floor overall slopes away from the ridge axis. Gravity causes the elevated lithosphere at the ridge axis to push on the
Crystalline igneous rocks
triple junction
Graded bed
Ridge-push force
21. 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.
A-horizon
Continental drift evidence
Phreatomagmatic eruptions
Gem
22. 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.
Convective flow
Compaction
Volatiles
Ultramafic
23. Low-viscosity (basaltic) lava flows out of a volcano easily - whereas high-viscosity (andesitic and rhyolitic) lava can clog and build pressure within a volcano. Basaltic eruptions are typically effusive and produce shield volcanoes - whereas rhyolit
The effect of viscosity on eruptive style
Lithosphere
Basaltic lava flows
Fracture zones
24. Rock formations still attached to the Earth's crust.
Alloy
Fumerolic mineralization
Soil Horizons
Bedrock
25. Cause of melting; magma can also form at locations where chemicals called volatiles mix with hot mantle rock. Elements such as water and carbon dioxide mix with hot rock - helping to break chemical bonds - so that if you add volatiles to a solid - ho
Bed
Native metals
Volatiles
Organic sedimentary rocks
26. Chemical weathering during Which minerals dissolve into water.
Dissolution
Laccolith
Slab-pull force
Rock composition
27. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Hydration
Explosive eruptions
Hot-spot track
Deposition
28. 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.
Cementation
Marine magnetic anomaly
Physical weathering
B-horizon
29. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Streak
Shield volcano
Calderas
Explosive eruptions
30. 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
Earth's atmosphere
Phreatomagmatic eruptions
Chemical weathering
Slab-pull force
31. A sediment-filled depression; in an area where the lithosphere has subsided.
Sedimentary Basins
Hydration
Regression
Subsidence
32. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Fissure eruptions/lava plateaus
Continental shelf
ravertine
Heat transfer
33. The transformation of loose sediment into solid rock.
Intermediate
Lithification
Dunes
Luster
34. 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.
Transform plate boundary
Basalt
Carbonate rocks
Saprolite
35. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Marine magnetic anomaly
Bedding
Biomineralization
Special properties of minerals
36. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Color
Grain sizes
E-horizon
Large Igneous Provinces (LIPs)
37. Type of soil; forms directly from underlying bedrock.
Lithosphere
Residual soil
Dunes
Basalt
38. 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.
Cinder cone
Deposition
Erosion
Plate tectonics
39. An insulated - tunnel-like conduit through which lava moves within a flow.
Volcanic pipes/necks
Lava tube
Erosion
Biochemical sedimentary rocks
40. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
The effect of viscosity on eruptive style
Rock texture
Native metals
Outcrop
41. The injection of magma within the magma chamber and conduit generates an outward pressure within the volcano. The presence of gas within the magma increases this pressure - as gas expands greatly as it rises toward the Earth's surface. Rhyolitic and
Rhyolitic lava flows
Rock-forming silicate minerals
A-horizon
The effect of gas pressure on eruptive style
42. 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.
Graded bed
Glassy igneous rocks
Rocks
Paleomagnetism
43. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Felsic - intermediate - mafic - ultramafic
Laccolith
Flood basalts
Symmetry
44. 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
Lower mantle
Pangaea
Loam
Crystal
45. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Convergent plate boundary
Effusive eruptions
Ultramafic
Bedding
46. Two different minerals which have the same composition but have different crystal structures.
Five steps of clastic sedimentary rock formation
Polymorphs
Magma mixing
Transgression
47. A mineral's growth that is uninhibited - has well-formed crystal faces.
Pangaea
Volcanic blocks/bombs
Euhedral crystal
Tuff
48. Forms when clots of lava fly into the air in lava fountains and then freeze to form solid chunks before hitting the ground. Some forms when the explosion of a volcano shatters preexisting rock and ejects the fragments over the countryside.
Pyroclastic debris
Volcano
Why magma rises
Rocks
49. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Abyssal plains
Lava
Sedimentary rocks
Tuff
50. Mineral group; feldspars - quartz - muscovite - clay minerals.
Magnetic declination
Granitic composition
Magnetic inclination
Light silicates