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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. 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
Crystal
Regression
Facets
Partial melting
2. 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.
Clastic
Why magma rises
Zone of accumulation
Convergent plate boundary
3. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Alloy
The effect of viscosity on eruptive style
Source rock composition
Ultramafic
4. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Transform plate boundary
Sedimentary structure
Ignimbrite
Basaltic lava flows
5. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Tephra
Mid-ocean ridges
Seamount chains
Xenolith
6. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Crystal
Soil Horizons
Luster
Laccolith
7. 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.
Inner core
pahoehoe
Rocks
Explosive eruptions
8. Molten rock beneath Earth's surface.
Zone of leaching
Magma
Fissure eruptions/lava plateaus
Intermediate
9. 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.
Xenolith
rifting
Pyroclastic debris
Solid-state diffusion
10. 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.
Grain sizes
Rock-forming silicate minerals
3.5km (2 miles)
The core
11. Distinguishing feature of magma; the process where magma changes composition as it cools because formation and sinking of crystals preferentially remove certain atoms from the magma.
Decompression
Fractional crystallization
Magnetic reversals
Frost wedging
12. 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.
Chemical weathering
Oxides
Halides
ravertine
13. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
atmospheres (atm)
Crystalline igneous rocks
C-horizon
Facets
14. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Clastic sedimentary rocks
Composite cone (stratovolcano)
Dunes
Viscosity
15. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Sulfides
Calderas
Hydrosphere
Quartz sandstone
16. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Erosion
Transported soil
Magma
Ripples
17. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Oxides
ravertine
Clastic
Carbonate rocks
18. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Columnar jointing
Lower mantle
Ridge-push force
Stratagraphic formation
19. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
The effect of gas pressure on eruptive style
Fracture and cleavage
Mineral
Inner core
20. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Magnetic anomaly
Laccolith
Crystalline igneous rocks
Plates
21. 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 -
Carbonates
Volcano
Graded bed
Mid-ocean ridges
22. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Magnetic reversals
Gabbro
Soil
Marine magnetic anomaly
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
Upper mantle
Flood basalts
Sedimentary structure
The effect of viscosity on eruptive style
24. 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.
Alloy
Symmetry
Silicate minerals
C-horizon
25. 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
Factors of magma cooling time
Superplumes
Viscosity
Seamount chains
26. 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.
Plate tectonics
Large Igneous Provinces (LIPs)
650-1100 degrees C
B-horizon
27. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Assimilation
Lapilli
Pyroclastic flows
Erosion
28. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Limestone
Sulfides
Area of igneous activity
Cement
29. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Regolith
Andesitic lava flows
Deep-ocean trenches
Dike
30. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Thermal expansion
Plates
Crystalline
31. 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.
Grain sizes
Relative plate velocity
Gem
Basalt
32. Physical property of a mineral; different minerals fracture in different ways - depending on the internal arrangement of atoms. If a mineral breaks to form distinct planar surfaces that have a specific orientation in relation to the crystal structure
Fracture and cleavage
Tuff
Cross beds
Transform fault
33. Deeper sublayer of the mantle - depth of 660km to 2900km.
Volatiles
Symmetry
Lower mantle
Melting
34. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Heat transfer
Redbeds
Glassy igneous rocks
Bed
35. 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.
Phreatomagmatic eruptions
Graded bed
Felsic - intermediate - mafic - ultramafic
Organic sedimentary rocks
36. An exposure of bedrock.
Regression
Outcrop
Facets
Conchoidal fractures
37. Sedimentary rock composed of quartz.
Siliceous rocks
Intrusive igneous rock
Divergent plate boundary
Ignimbrite
38. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Magnetic reversals
Granitic composition
Volcanic blocks/bombs
Jointing
39. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Extrusive igneous rock
Basaltic composition
Relative plate velocity
Chert
40. 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.
Partial melting
Crust
Metals
Sulfates
41. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Sea-floor spreading
Upper mantle
The effect of the environment on eruptive style
Silicate minerals
42. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Compaction
Paleomagnetism
Dark Silicates
Limestone
43. 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.
Upper mantle
Hydration
Magma mixing
Fumerolic mineralization
44. The base of the soil profile; consists of material derived from the substrate that's been chemically weathered and broken apart - but has not yet undergone leaching or accumulation.
Magnetic inclination
Continental rift
Zone of accumulation
C-horizon
45. Sedimentary rocks made up of the shells of organisms.
Plates
Native metals
Lava
Biochemical sedimentary rocks
46. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Crystalline igneous rocks
Weathering
a'a'
Arkose
47. An insulated - tunnel-like conduit through which lava moves within a flow.
Lava tube
Sandstone
Tuff
Viscosity
48. 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.
Root wedging
O-horizon
Silicates
Cinder cone
49. 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.
Compaction
Bedrock
Calderas
Clastic
50. Created from preexisting rocks which undergo changes - such as the growth of new minerals in response to pressure and heat - and/or as a result of squashing - stretching - or shear.
Physical weathering
Jointing
Relative plate velocity
Metamorphic rocks