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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. 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.
Hydration
Hydrosphere
Limestone
Fumerolic mineralization
2. A mineral's growth that is uninhibited - has well-formed crystal faces.
Magma mixing
Basaltic magma
Euhedral crystal
a'a'
3. 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
Transform plate boundary
Silicate minerals
rifting
Halides
4. 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
A-horizon
Viscosity
Metamorphic foliation
Residual soil
5. 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.
Sedimentary rocks
Decompression
Paleomagnetism
Glassy igneous rocks
6. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Chert
Asthenosphere
Intrusive igneous rock
Sedimentary rocks
7. 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
Redbeds
Phreatomagmatic eruptions
Ridge-push force
8. A sediment-filled depression; in an area where the lithosphere has subsided.
Zone of accumulation
Sedimentary Basins
Why magma rises
Strata
9. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Marine magnetic anomaly
Zone of accumulation
Ultramafic
Depositional environment
10. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Euhedral crystal
Erosion
Deposition
Slab-pull force
11. Molten rock beneath Earth's surface.
Geothermal gradient
Magma
Assimilation
Zone of accumulation
12. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Caliche
650-1100 degrees C
Soil erosion
Cross beds
13. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Color
Ignimbrite
Basalt
Carbonates
14. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Weathering
Bathymetry
Explosive eruptions
15. Heat from an intense surface fire bakes and expands the outer layer of the rock. On cooling - the layer contracts - causing the outer part of the rock spall - or break off in sheet-like pieces.
Gabbro
Thermal expansion
Mineral crystal destruction
Oxidation
16. Physical features of the land surface represented by changes in elevation.
Rock layering
Topography
Magma
Coal
17. The burial and lithification of angular or rounded clasts form these types of rocks.
Conglomerate
Bed
Saprolite
Sea-floor spreading
18. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Crystal lattice
Deposition
Peridotite
Lower mantle
19. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Continental drift evidence
Native metals
Inner core
Conchoidal fractures
20. 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.
Tuff
Stoping
Sulfides
Seamount chains
21. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Crystal
Turbidite
The effect of the environment on eruptive style
Columnar jointing
22. Layering in metamorphic rocks.
Magma mixing
Polymorphs
Metamorphic foliation
Divergent plate boundary
23. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
pahoehoe
Continental rift
Continental shelf
Sulfates
24. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Magnetic inclination
Metamorphic rocks
Weathering
Limestone
25. A submarine suspension of sediment.
Subduction
Clastic
Sedimentary rocks
Turbidity current
26. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
Special properties of minerals
Partial melting
B-horizon
Ridge-push force
27. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
650-1100 degrees C
Laccolith
Zone of accumulation
Evaporites
28. 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.
Conglomerate
The effect of gas pressure on eruptive style
Jointing
Magnetic inclination
29. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Specific gravity
Root wedging
Granite
Ripples
30. 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.
Sulfates
Diagenesis
Cinder cone
Hydrosphere
31. 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.
collision
Pyroclastic debris
Rhyolitic lava flows
triple junction
32. Type of volcano; most are adjacent to the Pacific - larger in size - interbedded lavas and pyroclastics - consist of alternating layers of lava and tephra - most violent type of activity - may produce nuee ardente or lahars.
Igneous rocks
Composite cone (stratovolcano)
Viscosity
Divergent plate boundary
33. A sheet of tuff formed from a pyroclastic flow.
Hardness
Carbonate rocks
Bedding
Ignimbrite
34. Alfred Wegener's suggestion that the positions of the continents change through time as they drift away from each other. The flaw was that he lacked a plausible moving mechanism.
Continental drift hypothesis
Fragmental igneous rocks
Crystal
Geothermal gradient
35. Process where a convergent boundary ceases to exist when a piece of buoyant lithosphere - such as a continent or island arc - moves into the subduction zone. Yield some of the most spectacular mountains/mountain ranges on the planet including the Him
12km
Loam
collision
Alloy
36. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Dissolution
Plutons
Sandstone
Granitic magma
37. Distinguishing feature of magma; the process where different magmas formed in different locations from different sources may come in contact within a magma chamber prior to freezing. Thus the originally distinct magmas mix to create a new - different
Why magma rises
Hot spots
Area of igneous activity
Magma mixing
38. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Gabbro
Phreatomagmatic eruptions
Transition zone
Rock layering
39. 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
Diagenesis
Streak
Transition zone
Fracture zones
40. The most common minerals in the Earth. Contain silica (SiO2) mixed in varying proportions with other elements (typically iron - magnesium - aluminum - calcium - potassium - and sodium).
Silicate minerals
Rhyolitic lava flows
Mantle
Magma mixing
41. 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.
Native metals
Dark Silicates
Crust
Crystal habit
42. 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.
Crystal habit
Spreading rate
Phreatomagmatic eruptions
Erosion
43. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Stoping
Pyroclastic flows
Magma's speed of flow
Siltstone and mudstone
44. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Crystalline
Magnetic inclination
Melting
Lapilli
45. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Outcrop
Silicate minerals
Marine magnetic anomaly
Dark Silicates
46. The boundary between two beds is a bedding plane; several beds constitute this structure.
Strata
Polymorphs
Tephra
Volatiles
47. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
3.5km (2 miles)
Plates
Cinder cone
The effect of viscosity on eruptive style
48. Sea-floor spreading proponents - Hess and others realized that in order for the circumference of the Earth to remain constant through time - ocean floor must eventually sink back into the mantle. This sinking process consumes the ocean floor between
12km
Subduction
A-horizon
Fragmental igneous rocks
49. Rocks whose crystals interlock with each other.
Stoping
Mineral crystal destruction
Crystalline
Volatiles
50. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Shield volcano
Glass
Lower mantle
Xenolith