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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. Molten rock that has flowed out onto Earth's surface.
Large Igneous Provinces (LIPs)
Chemical weathering
Jointing
Lava
2. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Clastic sedimentary rocks
Transform plate boundary
Elemental composition of Earth
Paleopole
3. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Asthenosphere
Facets
Ignimbrite
Halides
4. 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.
Symmetry
Viscosity
Seamount chains
Upper mantle
5. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Rock composition
Sulfates
Chemical weathering
Continental shelf
6. 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.
Color
Soil
collision
Explosive eruptions
7. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Stratagraphic formation
Coal
Organic sedimentary rocks
Subsidence
8. 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.
Divergent plate boundary
Asthenosphere
Quartz sandstone
Specific gravity
9. A single - continuous (uninterrupted) piece of a crystalline solid bounded by flat surfaces called crystal faces that grew naturally as the mineral formed. Come in a variety of shapes - cubes - trapezoids - pyramids - octahedrons - hexagonal columns
The core
Crystal
3.5km (2 miles)
Graded bed
10. Some rocks develop their magnetization - their ability to produce a magnetic field - at the time that the rocks themselves formed. Such rocks - preserve a record of the Earth's magnetic field at known times in the past.
Paleomagnetism
Bed
Mantle plume
Carbonates
11. Contributes to formation of soil; occurs when rainwater percolates through the debris and carries dissolved ions and clay flakes downward - This is the region where the downward transport occurs.
Plutons
Mantle plume
Topography
Zone of leaching
12. A sediment-filled depression; in an area where the lithosphere has subsided.
Volcano
Basaltic magma
Sedimentary Basins
Magnetic reversals
13. Layering in metamorphic rocks.
Turbidity current
Metamorphic foliation
Why magma rises
Crust
14. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Heat transfer
Biomineralization
Batholiths
Factors classifying clastic sedimentary rocks
15. An insulated - tunnel-like conduit through which lava moves within a flow.
Assimilation
Dolostone
Lava tube
Mantle
16. Because different soil-forming processes operate at different depths - soils typically develop into these distinct zones. These zones can be arranged vertically into a soil profile.
Laccolith
Transported soil
Laterite
Soil Horizons
17. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Cementation
Plates
Lapilli
Regression
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.
Why magma rises
Shield volcano
Mafic
Luster
19. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Special properties of minerals
Carbonates
Factors of magma cooling time
Laterite
20. 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.
Ridge-push force
Pyroclastic flows
Magnetic declination
Metamorphic rocks
21. 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.
Tuff
Magnetic inclination
Agrillaceous rocks
Xenolith
22. The intrusion of numerous plutons in a region - produces a vast composite body that may be several hundred kilometers long and over 100km wide; an immense body of igneous rock.
Batholiths
Volcanic blocks/bombs
Rock texture
Large Igneous Provinces (LIPs)
23. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Clastic sedimentary rocks
Halides
Polymorphs
Chemical weathering
24. Type of soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
Sulfates
Mineral crystal destruction
Conchoidal fractures
Laterite
25. 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
Transported soil
Dipole
Crystal lattice
Redbeds
26. On a gem are the ground and polished surfaces made with a certain type of machine.
Agrillaceous rocks
Subsidence
Facets
Soil Horizons
27. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Quartz sandstone
Alloy
Lithosphere
Factors classifying clastic sedimentary rocks
28. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Basaltic composition
Zone of leaching
Sill
Tuff
29. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Fragmental igneous rocks
Depositional environment
Gem
Evaporites
30. 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.
Relative plate velocity
Cross beds
Ultramafic
Bedding
31. Fluid basaltic lava extruded from crustal fractures called fissures.
Fissure eruptions/lava plateaus
Continental shelf
Heat transfer
Continental drift hypothesis
32. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Dark Silicates
Volcanic blocks/bombs
Volcano
Rock-forming silicate minerals
33. The process by which sediment settles out of the transporting medium.
Differential weathering
Deposition
Zone of accumulation
Transform fault
34. 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.
Rock-forming silicate minerals
Erosion
Dissolution
A-horizon
35. 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
Lithification
Divergent plate boundary
Large Igneous Provinces (LIPs)
36. 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.
Granite
Volatiles
Solid-state diffusion
Rocks
37. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Lapilli
Metamorphic foliation
Andesitic lava flows
Tephra
38. Mineral group; feldspars - quartz - muscovite - clay minerals.
Light silicates
collision
Igneous rocks
Deposition
39. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Gem
Specific gravity
Cinder cone
Glassy igneous rocks
40. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Transform fault
Chert
Soil
Earth's atmosphere
41. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Intrusive igneous rock
Frost wedging
Conchoidal fractures
Fumerolic mineralization
42. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
B-horizon
Granite
Conglomerate
Transported soil
43. Form when solid materials become hot and transform into liquid - example - molten rock.
Cement
triple junction
Melts
Glassy igneous rocks
44. 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
Mineral
Zone of leaching
Clastic
45. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Seamount chains
Siliceous rocks
Precipitation
Sill
46. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Granitic magma
Chert
Xenolith
Dipole
47. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Polymorphs
Sedimentary Basins
Dunes
Heat transfer
48. 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.
Bedrock
Transgression
Volatiles
Fragmental igneous rocks
49. Places with particularly voluminous quantities of magma erupting or intruding.
Large Igneous Provinces (LIPs)
Euhedral crystal
Arkose
Pyroclastic flows
50. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Mineral
Sulfides
Bedrock
atmospheres (atm)