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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. Mineral crystal formation type; form by type of diffusion - the movement of atoms or ions through a solid to arrange into a new crystal structure; process takes place very slowly.
Rock texture
Erosion
Felsic - intermediate - mafic - ultramafic
Solid-state diffusion
2. The crust moves away from the Mid-Atlantic Ridge axis at a rate of 1cm per year. This velocity of sea-floor spreading is determined by the relationship between the paleomagnetic anomaly-stripe's width and the reverse polarity duration - the data reve
Carbonate rocks
Plate tectonics
Sedimentary Basins
Spreading rate
3. The freely pivoting up and down compass needle's angle of tilt relative to the location upon the Earth's surface. At the equator - the specialized magnetic needle would position horizontally and at a magnetic pole it would point straight down.
Gem
Abyssal plains
Magnetic inclination
The effect of viscosity on eruptive style
4. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Erosion
Fracture zones
Granitic composition
Compaction
5. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Chert
Magma's speed of flow
Continental drift evidence
Alloy
6. Distinct internal laminations within a ripple or dune that are inclined at an angle to the boundary of the main sedimentary layer. Form as a consequence of the evolution of dunes or ripples.
Bed
Area of igneous activity
Cross beds
Divergent plate boundary
7. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Magma mixing
Subduction
Plates
Hydrosphere
8. 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.
Rock texture
Carbonates
Intermediate
Sea-floor spreading
9. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Agrillaceous rocks
Asthenosphere
Sandstone
Melting
10. 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.
Dissolution
Chemical sedimentary rocks
Asthenosphere
Magma
11. 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.
O-horizon
Volatiles
Assimilation
Mafic
12. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Lapilli
Siliceous rocks
Plutons
Dissolution
13. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Soil
Silicate minerals
Crystal lattice
Gabbro
14. Fluid basaltic lava extruded from crustal fractures called fissures.
Silicate minerals
Subduction
Area of igneous activity
Fissure eruptions/lava plateaus
15. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Organic sedimentary rocks
Silicates
Continental rift
Soil erosion
16. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Silicate minerals
Hardness
Volcanic blocks/bombs
Superplumes
17. Tree roots that grow into joints can push those joints open in this process.
Special properties of minerals
Graded bed
Root wedging
Flood basalts
18. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Hydrolysis
Seamount chains
Quartz sandstone
Mafic
19. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Paleopole
Crust
Andesitic lava flows
Metamorphic foliation
20. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Symmetry
Composite cone (stratovolcano)
Fracture zones
Volcano
21. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Bedding
Salt wedging
Sedimentary structure
Color
22. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Pyroclastic flows
Limestone
Sedimentary Basins
Magma
23. 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.
Ash
Soil
Luster
Columnar jointing
24. The process by which sediment settles out of the transporting medium.
Deposition
Compaction
B-horizon
Cross beds
25. Sedimentary rocks consisting of carbon-rich relicts of plants.
Organic sedimentary rocks
Rock-forming silicate minerals
Volcano
Laterite
26. 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 -
Extrusive igneous rock
Granitic composition
Rock composition
Mid-ocean ridges
27. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Strata
Subduction
Specific gravity
Chert
28. When silt and clay accumulate in the flat areas bordering a stream - lagoon - or delta - the silt when lithified becomes this type of sediment. And the mud - when lithified - becomes another type of sediment - also known as shale.
Factors of magma cooling time
Hydrolysis
Coal
Siltstone and mudstone
29. 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
Loam
Magnetic anomaly
Rock composition
Partial melting
30. Cause of melting; when magma rises up from the mantle into the crust - it brings heat with it which raises the temperature of the surrounding crustal rock - and in some cases melting occurs.
Biochemical sedimentary rocks
Tuff
Asthenosphere
Heat transfer
31. An exposure of bedrock.
Hot-spot track
Outcrop
Tuff
Mantle plume
32. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Facets
Seamount chains
O-horizon
Arkose
33. Core division; between 2900 and 5155km deep. Liquid iron alloy - it exists as a liquid because the temperature here is so high that even the great pressures squeezing the region cannot lock atoms into a solid framework. This liquid iron alloy is able
Outer core
The effect of gas pressure on eruptive style
650-1100 degrees C
Spreading rate
34. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Viscosity
Basaltic lava flows
Crystal habit
Rock texture
35. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Ignimbrite
Sill
Lava domes
Oxidation
36. Forms a 2885-km-thick layer surrounding the core. In terms of volume - it is the largest part of the Earth. It consists entirely of ultramafic rock - peridotite.
Hot spots
Mantle
The effect of the environment on eruptive style
Asthenosphere
37. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Phreatomagmatic eruptions
Evaporites
Sedimentary Basins
Mafic
38. An insulated - tunnel-like conduit through which lava moves within a flow.
Paleomagnetism
Hydrolysis
Lava tube
atmospheres (atm)
39. 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.
Sulfides
Shield volcano
Zone of leaching
Sill
40. 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.
Caliche
Extrusive igneous rock
Halides
Factors of magma cooling time
41. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Reason for Earth's internal heat
Caliche
Granite
Salt wedging
42. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Calderas
Basaltic composition
Ultramafic
Mafic
43. 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
Plate tectonics
Soil erosion
Apparent polar-wander path
Magnetic declination
44. 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.
Turbidity current
Biomineralization
Lithification
Oxides
45. 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.
Intermediate
Transform plate boundary
Mantle plume
Compaction
46. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Ultramafic
Lithosphere
Clastic sedimentary rocks
Color
47. Process occurring in arid climates - dissolved salt in groundwater precipitates and grows as crystals in open pore spaces in rocks. This process pushes apart the surrounding grains and so weakens the rock that when exposed to wind or rain - the rock
Cementation
Salt wedging
Organic chemicals
Volcano
48. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
a'a'
Intrusive igneous rock
C-horizon
Crystal
49. 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).
Flood basalts
Bathymetry
Cementation
Transform plate boundary
50. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Lava tube
Asthenosphere
O-horizon
Hydration