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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. 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.
Transform plate boundary
650-1100 degrees C
Factors classifying clastic sedimentary rocks
Carbonate rocks
2. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Pangaea
Lithosphere
Apparent polar-wander path
Felsic - intermediate - mafic - ultramafic
3. 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
Deep-ocean trenches
Sedimentary rocks
Phreatomagmatic eruptions
4. 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.
Lava
Crust
Basalt
Oxides
5. 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).
Cementation
Clastic sedimentary rocks
Sill
Relative plate velocity
6. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
O-horizon
Columnar jointing
B-horizon
Crystal lattice
7. The removal of soil by running water or by wind.
Sill
Ripples
Magma
Soil erosion
8. 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.
collision
Rock texture
Earth's atmosphere
Grain sizes
9. Factors; the depth of the intrusion - the deeper - the more slowly it cools. The shape and size of a magma body - the greater the surface area - the faster it cools. The presence of circulating groundwater - water passing through cools magma faster.
Frost wedging
3.5km (2 miles)
Shield volcano
Factors of magma cooling time
10. The burial and lithification of angular or rounded clasts form these types of rocks.
Heat transfer
Conglomerate
Basalt
Magma mixing
11. Soil section below the A-horizon; a soil level that has undergone substantial leaching but has not yet mixed with organic material. Because it lacks organic materials - this horizon tends to be lighter than the A-horizon. Part of the zone of leaching
Bedrock
E-horizon
Earth's atmosphere
Mineral crystal destruction
12. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Tuff
Continental drift hypothesis
Silicate minerals
Chert
13. 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.
Soil Horizons
Andesitic lava flows
Color
Mantle
14. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Caliche
Transported soil
Continental shelf
Dark Silicates
15. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
ravertine
The core
Basaltic lava flows
C-horizon
16. Soil section below the O-horizon - humus has decayed further and has mixed with mineral grains (clay - silt - and sand). Water percolating through this horizon causes chemical weathering reactions to occur and produces ions in solution and new clay m
Rock composition
Crystalline
Tephra
A-horizon
17. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Physical weathering
Basaltic magma
ravertine
Graded bed
18. Layering in sedimentary rocks.
Conchoidal fractures
A-horizon
atmospheres (atm)
Bedding
19. 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
Intermediate
Large Igneous Provinces (LIPs)
Volcanic pipes/necks
20. 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.
Chert
Pangaea
Luster
Diagenesis
21. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Fragmental igneous rocks
Five steps of clastic sedimentary rock formation
Effusive eruptions
Columnar jointing
22. 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.
Dunes
Ridge-push force
Thermal expansion
Clastic sedimentary rocks
23. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Laccolith
Columnar jointing
Arkose
Facets
24. 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.
Magma mixing
Heat transfer
Fissure eruptions/lava plateaus
Pyroclastic debris
25. 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
Fumerolic mineralization
Inner core
Fissure eruptions/lava plateaus
Continental rift
26. Molten rock that has flowed out onto Earth's surface.
C-horizon
Lava
Lava domes
Magma mixing
27. When different rocks in an outcrop undergo weathering at different rates.
Conchoidal fractures
Chert
Felsic - intermediate - mafic - ultramafic
Differential weathering
28. Distinguishing feature of magma; the composition of the melt reflects the composition of the solid from which it was derived. Not all magmas form from the same source rock - therefore not all magmas have the same compositions.
Root wedging
Source rock composition
Mineral
Gem
29. A mineral's growth that is uninhibited - has well-formed crystal faces.
Euhedral crystal
Intermediate
Salt wedging
Divergent plate boundary
30. 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.
Composite cone (stratovolcano)
Sill
Rock layering
Mineral crystal destruction
31. 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.
Volcano
Basaltic composition
Sedimentary rocks
Diagenesis
32. 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.
Metamorphic foliation
Pyroclastic flows
Symmetry
Turbidity current
33. 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
Subduction
Hardness
Hydrolysis
Apparent polar-wander path
34. 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.
Zone of accumulation
Tephra
Dunes
Tuff
35. 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.
Granitic composition
Partial melting
Granitic magma
Rhyolitic lava flows
36. When silt and clay accumulate in the flat areas bordering a stream - lagoon - or delta - the silt when lithified becomes this type of sediment. And the mud - when lithified - becomes another type of sediment - also known as shale.
Magma
Viscosity
Crust
Siltstone and mudstone
37. The rate of increase in temperature - decreases with increasing depth. The dashed lines represent the solidus and liquidus for mantle rock (peridotite). The solidus line defines the conditions of pressure and temperature at Which mantle rock begins t
Volatiles
Tuff
Geothermal gradient
Mantle plume
38. The boundary between two beds is a bedding plane; several beds constitute this structure.
650-1100 degrees C
Why magma rises
Cementation
Strata
39. On a gem are the ground and polished surfaces made with a certain type of machine.
Convective flow
Pangaea
Bed
Facets
40. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Subduction
Rock layering
Fissure eruptions/lava plateaus
Elemental composition of Earth
41. 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
Zone of accumulation
Marine magnetic anomaly
Melting
Crystal habit
42. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
The effect of gas pressure on eruptive style
Crystal habit
Crystal lattice
Asthenosphere
43. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Rock layering
Soil
Sandstone
Conglomerate
44. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Soil erosion
Plutons
Hardness
Sill
45. Fluid basaltic lava extruded from crustal fractures called fissures.
Fissure eruptions/lava plateaus
Paleopole
atmospheres (atm)
Subduction
46. 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
Volcano
Mineral crystal destruction
Outer core
Relative plate velocity
47. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Continental rift
Physical weathering
Mineral crystal destruction
Oxidation
48. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Mineral crystal destruction
Seamount chains
Fragmental igneous rocks
Outer core
49. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Abyssal plains
Weathering
Crystalline igneous rocks
Effusive eruptions
50. A plate boundary at which one plate slips along the side of another plate. No new plate is formed and no old plate is consumed. But the grinding between the plates generates frequent and destructive earthquakes.
O-horizon
Weathering
Metamorphic rocks
Transform plate boundary