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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. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Quartz sandstone
Light silicates
Andesitic lava flows
Clastic sedimentary rocks
2. 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.
Convective flow
Pyroclastic debris
Siltstone and mudstone
The effect of gas pressure on eruptive style
3. Sedimentary rock composed of calcite or dolomite.
Magma
Quartz sandstone
Fracture zones
Carbonate rocks
4. By melting - dissolving - or other chemical reactions.
Partial melting
Mineral crystal destruction
Dipole
Ripples
5. Molten rock beneath Earth's surface.
Magma
Specific gravity
Mafic
Differential weathering
6. 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.
Regolith
Crystal lattice
Sedimentary Basins
Batholiths
7. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Dike
Sandstone
Limestone
Native metals
8. 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
Viscosity
Apparent polar-wander path
Solid-state diffusion
Marine magnetic anomaly
9. 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.
Deep-ocean trenches
Intermediate
Graded bed
Transition zone
10. Center of the Earth - consists mainly of iron alloy.
The core
Crust
Reason for Earth's internal heat
Volatiles
11. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Biomineralization
Plutons
Thermal expansion
Sill
12. 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.
Chert
Continental drift hypothesis
Facets
Crust
13. 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.
Root wedging
Siltstone and mudstone
Rock texture
Area of igneous activity
14. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Plutons
Lava domes
Intermediate
Pyroclastic debris
15. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Metamorphic foliation
Intrusive igneous rock
Granitic composition
Volcanic blocks/bombs
16. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Partial melting
Halides
Rock layering
Basaltic magma
17. A plate boundary at which two plates move toward one another so that one plate sinks beneath the other. Subduction zones; Engage the sinking process known as subduction - between plates - consuming old oceanic lithosphere due to high density. Can sim
Convergent plate boundary
Transported soil
Streak
Weathering
18. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Apparent polar-wander path
Granitic composition
Mafic
Felsic - intermediate - mafic - ultramafic
19. Times when the Earth's magnetic field flips from normal to reversed polarity - or vice versa. When the Earth has reversed polarity - the south magnetic pole lies near the north geographic pole - and the north magnetic pole lies near the south geograp
Mantle plume
Ridge-push force
Glass
Magnetic reversals
20. 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
Continental rift
Outer core
Frost wedging
Rock texture
21. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
Columnar jointing
Redbeds
Mantle plume
Cement
22. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Quartz sandstone
C-horizon
Laccolith
Transition zone
23. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Carbonate rocks
Igneous rocks
Transported soil
Differential weathering
24. 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.
Streak
Clastic sedimentary rocks
Oxides
Transition zone
25. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Soil erosion
Evaporites
Dunes
Ripples
26. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
pahoehoe
B-horizon
Hardness
Five steps of clastic sedimentary rock formation
27. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Streak
Seamount chains
Metamorphic rocks
Felsic
28. Some rock bodies appear to contain distinct formations - defined either by bands of different compositions or textures - or by the alignment of inequant grains so that they trend parallel to one another.
Dolostone
Spreading rate
Decompression
Rock layering
29. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Relative plate velocity
Soil erosion
Volcanic pipes/necks
Felsic - intermediate - mafic - ultramafic
30. 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
Mafic
Subsidence
Cement
Dipole
31. 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
Slab-pull force
Oxidation
Silicate minerals
Magma's speed of flow
32. 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.
Fragmental igneous rocks
Relative plate velocity
Composite cone (stratovolcano)
Caliche
33. Rocks which develop when hot molten rock cools and freezes solid.
Physical weathering
Volatiles
Igneous rocks
Carbonates
34. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Jointing
Andesitic lava flows
Oxides
Dolostone
35. Type of volcanic eruption; pyroclastic - produce clouds and avalanches of pyroclastic debris. Gas expands in the rising magma - cannot escape. The pressure becomes so great that it blasts the lava - and volcanic rock - out of the volcano.
Turbidite
Explosive eruptions
Plutons
Special properties of minerals
36. An envelope of gas surrounding Earth consisting of 78% nitrogen (N2) and 28% oxygen (O2) - with minor amounts 1% of argon - carbon dioxide - methane - etc. And 99% of the gas in the atmosphere lies below 50km.
37. 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
Laterite
E-horizon
Magnetic anomaly
Metamorphic foliation
38. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Glass
Oxidation
Deep-ocean trenches
Depositional environment
39. 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
Rocks
Assimilation
Calderas
40. 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.
12km
Continental drift evidence
Bathymetry
Heat transfer
41. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Bathymetry
Heat transfer
Ultramafic
Continental drift evidence
42. 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.
Weathering
Sulfates
Cement
Light silicates
43. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
650-1100 degrees C
Organic chemicals
Abyssal plains
Silicate minerals
44. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Area of igneous activity
Calderas
Continental drift evidence
Volcanic pipes/necks
45. A sediment-filled depression; in an area where the lithosphere has subsided.
Basalt
Volatiles
Sedimentary Basins
Hydrolysis
46. Two different minerals which have the same composition but have different crystal structures.
Effusive eruptions
Evaporites
Regolith
Polymorphs
47. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Batholiths
Metamorphic foliation
Native metals
Mineral
48. Process where new divergent boundaries form when a continent splits and separates into two continents.
rifting
Heat transfer
Inner core
Bathymetry
49. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Ash
Transform plate boundary
Granitic magma
Bed
50. 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
Granitic composition
Lithosphere
Asthenosphere