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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. Process where new divergent boundaries form when a continent splits and separates into two continents.
Soil erosion
Caliche
Metals
rifting
2. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Factors of magma cooling time
A-horizon
Thermal expansion
Sea-floor spreading
3. Rocks that forms by the freezing of lava above ground - after it spills out (extrudes) onto the surface of the Earth and comes into contact with the atmosphere or ocean.
A-horizon
Facets
Extrusive igneous rock
Pangaea
4. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Sill
Lapilli
Mantle
Saprolite
5. Places where intrusive igneous rock creates tabular intrusions cutting across rock that does not have layering - this nearly vertical - wall-like tabular intrusions is formed. Cut across layering within the earth.
Flood basalts
Graded bed
Native metals
Dike
6. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Native metals
Inner core
atmospheres (atm)
Ultramafic
7. 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
Andesitic lava flows
Five steps of clastic sedimentary rock formation
The effect of viscosity on eruptive style
Outer core
8. A fine spray of lava instantly freezes to form fine particles of glass.
Root wedging
Rock layering
Ash
Zone of leaching
9. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Residual soil
Sill
Lithosphere
Volatiles
10. 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.
atmospheres (atm)
Magnetic declination
Hydration
Luster
11. 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.
Graded bed
Ripples
Silicates
Batholiths
12. Weathering - erosion - transportation - deposition - and lithification.
Viscosity
Polymorphs
Five steps of clastic sedimentary rock formation
Volcanic pipes/necks
13. Refers to the arrangement of grains in a rock; that is - the way the grains connect each other and whether inequant grains are aligned parallel to one another.
12km
Intermediate
Limestone
Rock texture
14. 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
Siltstone and mudstone
Felsic - intermediate - mafic - ultramafic
Cross beds
15. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Magma
Hydration
Metamorphic rocks
Basalt
16. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Slab-pull force
Bed
Fumerolic mineralization
The core
17. Layering in sedimentary rocks.
Bedding
Dunes
Metamorphic foliation
Crystalline igneous rocks
18. The display of the pattern of atoms or ions within a mineral. Meaning that the shape of one part of a mineral is a mirror image of the shape of another part.
Luster
Symmetry
Slab-pull force
Polymorphs
19. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
Melting
Andesitic lava flows
Hydrosphere
B-horizon
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
Ridge-push force
Xenolith
Special properties of minerals
Intrusive igneous rock
21. Mineral group; feldspars - quartz - muscovite - clay minerals.
Alloy
Cinder cone
Light silicates
Transported soil
22. 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
Divergent plate boundary
Gabbro
Dissolution
23. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
rifting
650-1100 degrees C
Clastic sedimentary rocks
Lithosphere
24. A place where three plate boundaries intersect at a point.
triple junction
Geothermal gradient
Magnetic anomaly
Dissolution
25. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Dark Silicates
Columnar jointing
Solid-state diffusion
Intermediate
26. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Outer core
Sandstone
3.5km (2 miles)
Weathering
27. The record of paleomagnetism revealed that the location of Earth's magnetic poles had been changing through geologic time. This 'wandering' meant that Earth's magnetic poles do not move with respect to fixed continents. Rather - continents move relat
Fissure eruptions/lava plateaus
ravertine
Soil erosion
Apparent polar-wander path
28. 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.
Relative plate velocity
Oxides
Silicate minerals
Magma
29. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Thermal expansion
Fracture and cleavage
Transported soil
Transgression
30. Process where a convergent boundary ceases to exist when a piece of buoyant lithosphere - such as a continent or island arc - moves into the subduction zone. Yield some of the most spectacular mountains/mountain ranges on the planet including the Him
collision
Intermediate
Transition zone
Mineral
31. 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.
Deep-ocean trenches
Transition zone
Dissolution
Luster
32. 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.
Tephra
Bed
Fracture zones
Rock composition
33. Sedimentary rock composed of quartz.
Explosive eruptions
Root wedging
Siliceous rocks
Spreading rate
34. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Crystalline igneous rocks
Luster
Stoping
Melting
35. Molten rock beneath Earth's surface.
Native metals
Agrillaceous rocks
Magma
Redbeds
36. The boundary between two beds is a bedding plane; several beds constitute this structure.
Compaction
Strata
Metals
Fragmental igneous rocks
37. 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.
Basalt
Sedimentary structure
Silicate minerals
Pangaea
38. 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
Upper mantle
Crystal
Arkose
Viscosity
39. 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.
Soil
Divergent plate boundary
Dipole
Ripples
40. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Igneous rocks
Silicates
collision
Gabbro
41. Physical features of the land surface represented by changes in elevation.
Topography
Magnetic inclination
Large Igneous Provinces (LIPs)
Hydration
42. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Volcano
Magma mixing
Transition zone
Weathering
43. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Granitic composition
Carbonates
Zone of leaching
Volatiles
44. 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 -
Superplumes
Felsic
Transform plate boundary
Mid-ocean ridges
45. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Granite
Regolith
Conchoidal fractures
Grain sizes
46. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Glass
3.5km (2 miles)
Inner core
Andesitic lava flows
47. Fluid basaltic lava extruded from crustal fractures called fissures.
Sulfides
Luster
Fissure eruptions/lava plateaus
Metamorphic rocks
48. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Partial melting
Carbonates
Calderas
Columnar jointing
49. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Erosion
Phreatomagmatic eruptions
Basalt
Felsic - intermediate - mafic - ultramafic
50. 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.
Crystal
Sulfides
Fracture and cleavage
Graded bed