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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. Rocks whose crystals interlock with each other.
Fracture and cleavage
Crystalline igneous rocks
Crystalline
Lower mantle
2. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Turbidity current
Crystal structure
Pangaea
Sill
3. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Batholiths
Outer core
Silicate minerals
Sandstone
4. 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
Transform fault
The core
Topography
5. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
Decompression
Mantle plume
Hardness
Salt wedging
6. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Chemical sedimentary rocks
Sedimentary structure
Salt wedging
Transported soil
7. An insulated - tunnel-like conduit through which lava moves within a flow.
Siliceous rocks
Zone of accumulation
Fracture zones
Lava tube
8. Breaks intact rocks into unconnected grains or chunks - collectively called debris or detritus. Grain size from largest to smallest: boulders - cobbles - pebbles - sand - silt - mud/clay.
Melting
Subduction
Physical weathering
Plutons
9. The difference between the expected strength of the Earth's main field at a certain location and the actual measure strength of the magnetic field at that location. Places where the field strength is stronger that expected are positive anomalies - an
Magnetic anomaly
Sedimentary rocks
Area of igneous activity
Continental shelf
10. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Crystal lattice
Apparent polar-wander path
Frost wedging
11. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Lower mantle
Marine magnetic anomaly
Mineral
Salt wedging
12. After sand has lost its feldspar composition due to weathering over time - sediment composed entirely of quartz grains gets buried and lithified to form this type of rock.
Quartz sandstone
Why magma rises
Andesitic lava flows
Cross beds
13. 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
Oxidation
Ridge-push force
Outer core
Pyroclastic flows
14. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Andesitic lava flows
The effect of viscosity on eruptive style
Ignimbrite
Paleopole
15. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Convergent plate boundary
Biomineralization
Metamorphic rocks
Depositional environment
16. Outer surface level of Earth; composed of granite - basalt - and gabbro. Continental: mostly about 35-40km thick . Oceanic: about 7-10km thick. Oxygen - by far the most abundant element.
Crust
Volcano
Silicate minerals
Sulfates
17. 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.
Carbonate rocks
Heat transfer
Continental shelf
Volatiles
18. 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
Bedding
Five steps of clastic sedimentary rock formation
Effusive eruptions
19. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Subsidence
Intermediate
Conchoidal fractures
Turbidite
20. 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
Xenolith
Fracture zones
The effect of viscosity on eruptive style
Precipitation
21. 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
Transgression
Spreading rate
Why magma rises
Regolith
22. The process by which sediment settles out of the transporting medium.
Deposition
Lava tube
Lapilli
Volatiles
23. A submarine suspension of sediment.
Outer core
Color
Factors of magma cooling time
Turbidity current
24. The Earth radiated heat into space and slowly cooled. Eventually - the early formed sea of lava solidified and formed igneous rock. The cumulative effect of radioactivity has been sufficient to slow the cooling of the planet and subsequently allow fo
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25. 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
Hydrosphere
Symmetry
Loam
Silicate minerals
26. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Elemental composition of Earth
Organic chemicals
Clastic sedimentary rocks
Mineral
27. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Volcanic blocks/bombs
Depositional environment
Plutons
Sulfates
28. 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
Decompression
Hot spots
Rock-forming silicate minerals
29. 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.
Intrusive igneous rock
Chemical sedimentary rocks
Zone of accumulation
Lithosphere
30. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
E-horizon
Hydrosphere
Factors classifying clastic sedimentary rocks
31. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Hot spots
Intermediate
Symmetry
Divergent plate boundary
32. Center of the Earth - consists mainly of iron alloy.
Crystalline igneous rocks
Effusive eruptions
The core
Chemical weathering
33. 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 -
Mid-ocean ridges
Plate tectonics
Bathymetry
Volcanic pipes/necks
34. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Biomineralization
Halides
Factors classifying clastic sedimentary rocks
Fumerolic mineralization
35. Physical property of a mineral; refers to the shape (morphology) of a single crystal with well-formed crystal faces - or to the character of an aggregate of many well-formed crystals that grew together as a group. Depends on the internal arrangement
Crystal habit
C-horizon
Tuff
atmospheres (atm)
36. Process where new divergent boundaries form when a continent splits and separates into two continents.
rifting
Laccolith
The effect of the environment on eruptive style
Tuff
37. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Hydration
Crystalline igneous rocks
Seamount chains
Magnetic declination
38. 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.
650-1100 degrees C
Mid-ocean ridges
Jointing
Plate tectonics
39. Deeper sublayer of the mantle - depth of 660km to 2900km.
Evaporites
Seamount chains
Polymorphs
Lower mantle
40. The burial and lithification of angular or rounded clasts form these types of rocks.
Evaporites
Soil
Organic sedimentary rocks
Conglomerate
41. Sedimentary rocks consisting of carbon-rich relicts of plants.
Basalt
Limestone
Organic sedimentary rocks
Oxides
42. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Rock composition
12km
Dike
Assimilation
43. 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).
O-horizon
Cementation
Lava tube
Viscosity
44. 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.
Phreatomagmatic eruptions
Dike
Granitic magma
Laterite
45. A fine spray of lava instantly freezes to form fine particles of glass.
Flood basalts
Crystal habit
Ash
triple junction
46. Weathering - erosion - transportation - deposition - and lithification.
Luster
Silicate minerals
Reason for Earth's internal heat
Five steps of clastic sedimentary rock formation
47. Rocks which develop when hot molten rock cools and freezes solid.
Color
Igneous rocks
Saprolite
Partial melting
48. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Rhyolitic lava flows
Turbidity current
Oxides
Source rock composition
49. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Weathering
Crystal lattice
Dolostone
Basaltic lava flows
50. 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
Gem
Dipole
Sedimentary Basins
Tuff