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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. Form when solid materials become hot and transform into liquid - example - molten rock.
Melts
Explosive eruptions
Dike
Light silicates
2. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Zone of leaching
Graded bed
E-horizon
Dunes
3. Weathering - erosion - transportation - deposition - and lithification.
Mineral crystal destruction
Five steps of clastic sedimentary rock formation
Intermediate
Metamorphic rocks
4. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Elemental composition of Earth
Fissure eruptions/lava plateaus
Apparent polar-wander path
Stoping
5. A sediment-filled depression; in an area where the lithosphere has subsided.
Rock layering
Soil
Sedimentary Basins
Ridge-push force
6. Type of igneous rock composition; composed of dark silicates and calcium-rich feldspar - referred to as mafic (magnesium and iron). Make up the ocean floor/volcanic islands.
Granitic composition
Regolith
Basaltic composition
Volcanic blocks/bombs
7. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Calderas
Subduction
Depositional environment
Turbidite
8. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Continental drift hypothesis
Convective flow
Hot-spot track
Mantle plume
9. 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).
Ripples
Depositional environment
Metals
Cementation
10. Sublayer of the mantle - depth of 660km.
Ridge-push force
Upper mantle
Ignimbrite
Ash
11. The combination of processes that separate rock or regolith from its substrate and carry it away. Involves abrasion - plucking - scouring - and dissolution - and is caused by air - water or ice.
Siliceous rocks
Carbonates
Erosion
Heat transfer
12. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Gabbro
Paleopole
Lava
Lapilli
13. Type of soil; forms directly from underlying bedrock.
Lava domes
Effusive eruptions
Ripples
Residual soil
14. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Compaction
Source rock composition
Explosive eruptions
Conchoidal fractures
15. 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.
Asthenosphere
Abyssal plains
Shield volcano
Subduction
16. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Caliche
Chert
Intermediate
Hydrosphere
17. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Sedimentary rocks
Metamorphic foliation
Ripples
Differential weathering
18. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Residual soil
Effusive eruptions
Zone of accumulation
Grain sizes
19. 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
Sandstone
Continental rift
Sea-floor spreading
Decompression
20. Mineral group; feldspars - quartz - muscovite - clay minerals.
Gem
Plates
Facets
Light silicates
21. A distinctive sequence of strata traced across a fairly large region. For example - a region may contain a succession of alternating sandstone and shale beds deposited by rivers - overlain by beds of marine limestone deposited later.
Granite
Mantle
Hot-spot track
Stratagraphic formation
22. 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.
Bedrock
Luster
Volatiles
Fractional crystallization
23. Physical property of a mineral; refers to the color of a powder produced by pulverizing the mineral. Provides a fairly reliable clue to the mineral's identity - since the color of the mineral powder tends to be less variable than the color of the who
Sea-floor spreading
Stratagraphic formation
Streak
Precipitation
24. Sedimentary rock composed of clay.
collision
Seamount chains
Intermediate
Agrillaceous rocks
25. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Turbidity current
Ripples
Biomineralization
Sill
26. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
A-horizon
Abyssal plains
Transform fault
Seamount chains
27. Along much of the perimeter of the Pacific Ocean - the ocean floor reaches astounding depths of 8-12km. These areas define elongate troughs - and they border volcanic arcs - the curving chains of active volcanoes.
Deep-ocean trenches
Paleopole
Source rock composition
Stratagraphic formation
28. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Hot spots
Composite cone (stratovolcano)
Frost wedging
Granitic magma
29. The shape of the sea floor surface. Investigation of the sea-floor revealed the presence of several important features: mid-ocean ridges - deep-ocean trenches - seamount chains - and fracture zones.
Mineral
Bathymetry
Zone of accumulation
Chemical weathering
30. 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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31. 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.
Mantle
Luster
Mantle plume
Coal
32. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Sedimentary Basins
Factors classifying clastic sedimentary rocks
Mineral
The effect of viscosity on eruptive style
33. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Crystalline igneous rocks
Turbidity current
Magnetic inclination
Precipitation
34. Mineral class; the fundamental component within these types of minerals in the Earth's crust is the silicon-oxygen tetrahedron anionic group - a silicon atom surrounded by four oxygen atoms that are arranged to define the corners of a tetrahedron - a
Gabbro
Chemical weathering
Geothermal gradient
Silicates
35. On a gem are the ground and polished surfaces made with a certain type of machine.
Facets
Lower mantle
Basalt
Intrusive igneous rock
36. Core division; from a depth of 5155km down to Earth's center at 6371km. A radius of about 1220km - is solid iron-nickel alloy - can reach temperature of 4700 degrees C. Solid in nature because of subjection to greater pressure - keeps atoms from wand
Grain sizes
Ash
Siltstone and mudstone
Inner core
37. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
3.5km (2 miles)
Gem
Erosion
Weathering
38. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Bedrock
Lithification
Andesitic lava flows
Crystal lattice
39. 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.
Ripples
Fragmental igneous rocks
Polymorphs
Large Igneous Provinces (LIPs)
40. 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.
Cinder cone
Apparent polar-wander path
Lava
The core
41. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Laterite
O-horizon
Luster
Precipitation
42. The process by which sediment settles out of the transporting medium.
Plutons
Deposition
Biomineralization
Color
43. 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.
Upper mantle
Magnetic inclination
Glassy igneous rocks
Outcrop
44. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Coal
Seamount chains
Ridge-push force
Hot spots
45. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Large Igneous Provinces (LIPs)
Stratagraphic formation
Conchoidal fractures
Intrusive igneous rock
46. 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.
Solid-state diffusion
Basaltic lava flows
Strata
Sulfates
47. The ocean floor is diced up by narrow bands of vertical fractures. Lie roughly at right angles to mid-ocean ridges - effectively segmenting the ridges into small pieces.
Evaporites
Elemental composition of Earth
Fracture zones
Continental shelf
48. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
Apparent polar-wander path
Dike
Seamount chains
pahoehoe
49. The angle between the direction that a compass needle points at a given location and the direction of the 'true' (geographic) north. Through this process - the magnetic poles never stray more than 15 degrees of latitude from the geographic pole.
Flood basalts
Calderas
Magnetic declination
Magnetic anomaly
50. 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.
Transition zone
Soil erosion
Superplumes
Weathering