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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; the process where magma sits in a magma chamber before completely solidifying - it may incorporate chemicals derived from the walls rocks of the chamber.
Assimilation
Dike
Weathering
Precipitation
2. Times when the Earth's magnetic field flips from normal to reversed polarity - or vice versa. When the Earth has reversed polarity - the south magnetic pole lies near the north geographic pole - and the north magnetic pole lies near the south geograp
Magnetic reversals
Alloy
Ignimbrite
B-horizon
3. A rock made of solid mass of glass - or of tiny crystals surrounded by glass. Reflect light as glass does and tend to break conchoidally. Examples - obsidian - tachylite - pumice.
Glassy igneous rocks
Light silicates
Silicate minerals
Cross beds
4. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Calderas
The core
Facets
Ultramafic
5. The transformation of loose sediment into solid rock.
Lithification
Transported soil
Diagenesis
Volatiles
6. Magma viscosity depends upon temperature - volatile content - and silica content. Hotter magma - more volatiles - and mafic magma all have less viscosity.
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7. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Caliche
Ripples
Turbidite
Salt wedging
8. A place where three plate boundaries intersect at a point.
triple junction
Strata
Turbidity current
Conglomerate
9. An insulated - tunnel-like conduit through which lava moves within a flow.
Extrusive igneous rock
Luster
Lava tube
Dissolution
10. 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
Subsidence
Symmetry
Batholiths
Spreading rate
11. Sedimentary rock composed of quartz.
Fracture and cleavage
Metamorphic rocks
Biochemical sedimentary rocks
Siliceous rocks
12. 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.
Clastic
Ignimbrite
Transition zone
Rock-forming silicate minerals
13. A sheet of tuff formed from a pyroclastic flow.
Rocks
Outcrop
Ignimbrite
Grain sizes
14. On a gem are the ground and polished surfaces made with a certain type of machine.
Coal
Bathymetry
Phreatomagmatic eruptions
Facets
15. 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.
Native metals
pahoehoe
Apparent polar-wander path
Cinder cone
16. 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
Outcrop
Sill
Ultramafic
17. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Plate tectonics
Turbidite
Bedrock
Graded bed
18. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Regression
Granitic magma
Viscosity
Bed
19. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Crystal lattice
Convergent plate boundary
Symmetry
Bedding
20. 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.
Seamount chains
Physical weathering
Dike
Fractional crystallization
21. 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
Bathymetry
Continental rift
Conchoidal fractures
22. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
3.5km (2 miles)
The effect of viscosity on eruptive style
Rock composition
Sedimentary structure
23. 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.
Streak
Dike
Outcrop
Phreatomagmatic eruptions
24. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Silicate minerals
Weathering
Seamount chains
Pyroclastic debris
25. Layering in sedimentary rocks.
Viscosity
Lower mantle
Peridotite
Bedding
26. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Hot-spot track
Pyroclastic debris
Magnetic reversals
Agrillaceous rocks
27. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
B-horizon
Source rock composition
Subsidence
Caliche
28. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Subsidence
Caliche
Hydrolysis
Carbonates
29. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Basaltic lava flows
Metamorphic foliation
Magnetic anomaly
Dunes
30. 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.
12km
Compaction
Oxides
Dipole
31. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Lapilli
Superplumes
Arkose
Hardness
32. 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.
Depositional environment
Silicate minerals
Bedding
650-1100 degrees C
33. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Granite
Lava tube
Sedimentary structure
Calderas
34. Physical features of the land surface represented by changes in elevation.
Topography
Inner core
12km
Diagenesis
35. A process occurring when sea level falls - the coast migrates seaward.
triple junction
Differential weathering
The effect of the environment on eruptive style
Regression
36. Molten rock that has flowed out onto Earth's surface.
Transgression
Lava
Ridge-push force
Stratagraphic formation
37. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Rock composition
Basaltic lava flows
Laccolith
Factors classifying clastic sedimentary rocks
38. 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
Intermediate
Lithification
Metamorphic rocks
Volatiles
39. 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.
Sill
Carbonate rocks
Diagenesis
Laccolith
40. 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
Peridotite
Area of igneous activity
Crystal structure
41. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Jointing
Volatiles
Continental shelf
Fragmental igneous rocks
42. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Salt wedging
Streak
Earth's atmosphere
Jointing
43. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Granite
Soil Horizons
Dike
Rock layering
44. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Conchoidal fractures
Granitic composition
Magma
Limestone
45. 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
Heat transfer
12km
collision
46. 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
3.5km (2 miles)
The effect of gas pressure on eruptive style
Earth's atmosphere
Salt wedging
47. 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
Crystalline
Soil Horizons
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.
Specific gravity
Alloy
Pyroclastic debris
Abyssal plains
49. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Mineral
Hot spots
Large Igneous Provinces (LIPs)
Symmetry
50. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Rock-forming silicate minerals
Clastic
A-horizon
Soil erosion