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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. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Magma mixing
Pangaea
Continental drift evidence
Melts
2. The speed of the movements of the plates with respect to the speed of the other plates' movements. Absolute plate velocity is a measure of the movement of any plates relative to a fixed point in the mantle.
Inner core
Relative plate velocity
Subduction
pahoehoe
3. Rocks which develop when hot molten rock cools and freezes solid.
Compaction
Organic chemicals
Gabbro
Igneous rocks
4. Sedimentary rock composed of quartz.
Siliceous rocks
Plates
Saprolite
Depositional environment
5. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Calderas
Lithosphere
Metamorphic rocks
Sedimentary structure
6. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Rock texture
Ultramafic
Loam
Zone of leaching
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.
O-horizon
Bed
Intrusive igneous rock
Subduction
8. A term used for all the physical - chemical - and biological processes that transform sediment into sedimentary rock and that alter characteristics of sedimentary rock one the rock has formed.
Dipole
Diagenesis
Silicate minerals
Limestone
9. Molten rock beneath Earth's surface.
Mafic
Magma
Sulfides
Source rock composition
10. 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.
Organic chemicals
Abyssal plains
Transition zone
Basaltic composition
11. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Clastic sedimentary rocks
Magma
Luster
Sulfates
12. Soil section below the A-horizon; a soil level that has undergone substantial leaching but has not yet mixed with organic material. Because it lacks organic materials - this horizon tends to be lighter than the A-horizon. Part of the zone of leaching
Phreatomagmatic eruptions
Subduction
Gem
E-horizon
13. Type of volcano; most are adjacent to the Pacific - larger in size - interbedded lavas and pyroclastics - consist of alternating layers of lava and tephra - most violent type of activity - may produce nuee ardente or lahars.
Lithosphere
Clastic sedimentary rocks
Composite cone (stratovolcano)
Lava tube
14. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Chemical weathering
Cross beds
Soil erosion
Pangaea
15. Places with particularly voluminous quantities of magma erupting or intruding.
Chert
Slab-pull force
Large Igneous Provinces (LIPs)
Divergent plate boundary
16. Type of volcano; built from ejected lava fragments - cone shaped piles of tephra - steep slope angle - smaller in size - frequently occur in groups - deep craters.
pahoehoe
Deep-ocean trenches
Cinder cone
Compaction
17. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Redbeds
Crystal
Physical weathering
Gem
18. Farther down from a zone of leaching - new mineral crystals precipitate directly out of the water or form when the water reacts with debris - this the region where the new minerals and clay collect.
Intermediate
Why magma rises
Slab-pull force
Zone of accumulation
19. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Columnar jointing
Hydrosphere
The effect of gas pressure on eruptive style
Basaltic magma
20. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
3.5km (2 miles)
12km
Stratagraphic formation
Ridge-push force
21. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Crystalline
Depositional environment
Columnar jointing
Reason for Earth's internal heat
22. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Lapilli
Quartz sandstone
Jointing
Intrusive igneous rock
23. Fluid basaltic lava extruded from crustal fractures called fissures.
Elemental composition of Earth
Fissure eruptions/lava plateaus
collision
Intermediate
24. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Decompression
Superplumes
A-horizon
Calderas
25. Type of volcano; broad and slightly domed - primarily made of basaltic lava - large and erupt large volumes of lava. Form from either low viscosity basaltic lava or from large pyroclastic sheets.
Shield volcano
Ridge-push force
Large Igneous Provinces (LIPs)
B-horizon
26. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Area of igneous activity
Flood basalts
Crystalline igneous rocks
Siliceous rocks
27. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Continental rift
Transgression
Chert
Limestone
28. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Laterite
Granitic composition
Sea-floor spreading
Hot-spot track
29. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Root wedging
Turbidite
Ripples
Decompression
30. The removal of soil by running water or by wind.
Soil erosion
Continental drift hypothesis
Plates
Partial melting
31. Heat from an intense surface fire bakes and expands the outer layer of the rock. On cooling - the layer contracts - causing the outer part of the rock spall - or break off in sheet-like pieces.
Topography
Thermal expansion
Seamount chains
Clastic sedimentary rocks
32. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Factors classifying clastic sedimentary rocks
Crystal habit
Volcanic blocks/bombs
Solid-state diffusion
33. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Hot-spot track
Asthenosphere
Continental shelf
Decompression
34. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Granitic composition
Asthenosphere
Dissolution
Conglomerate
35. Type of magma; low in silica - fluid - crystallize at high temperatures.
Magnetic declination
Basaltic magma
Organic sedimentary rocks
Crystal lattice
36. Physical features of the land surface represented by changes in elevation.
Graded bed
Facets
Topography
Erosion
37. 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.
Magma's speed of flow
Divergent plate boundary
Streak
Fragmental igneous rocks
38. The shape of the sea floor surface. Investigation of the sea-floor revealed the presence of several important features: mid-ocean ridges - deep-ocean trenches - seamount chains - and fracture zones.
Bathymetry
Composite cone (stratovolcano)
Salt wedging
Jointing
39. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Chemical weathering
Effusive eruptions
Pyroclastic flows
Hydration
40. 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.
Biochemical sedimentary rocks
Lava tube
Bathymetry
Transform plate boundary
41. 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.
Specific gravity
Sulfides
Slab-pull force
The effect of viscosity on eruptive style
42. 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
Peridotite
Transition zone
Lava
Apparent polar-wander path
43. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Continental shelf
ravertine
Continental drift evidence
Native metals
44. In degrees Celsius - the high temperatures at which igneous rocks freeze; the freezing of liquid melt to form solid igneous rock represents the same phenomenon as the freezing of water - except at much higher temperatures.
Pangaea
650-1100 degrees C
Igneous rocks
Siltstone and mudstone
45. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Fractional crystallization
Andesitic lava flows
Basalt
Columnar jointing
46. Mineral crystal formation type; from directly from a vapor - occurs around volcanic vents or around geysers. At such locations - volcanic gases or steam enter the atmosphere and cool - so certain elements cannot remain in gaseous form.
Fumerolic mineralization
Stratagraphic formation
Symmetry
E-horizon
47. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Tuff
Composite cone (stratovolcano)
Glass
Hot spots
48. 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
Convective flow
Chemical sedimentary rocks
Magma mixing
A-horizon
49. 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
Geothermal gradient
atmospheres (atm)
Sandstone
50. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Crystal structure
Fragmental igneous rocks
Erosion