SUBJECTS
|
BROWSE
|
CAREER CENTER
|
POPULAR
|
JOIN
|
LOGIN
Business Skills
|
Soft Skills
|
Basic Literacy
|
Certifications
About
|
Help
|
Privacy
|
Terms
|
Email
Search
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. Carbon-containing compounds that either occur in living organisms - or have characteristics that resemble the molecules within living organisms. Examples - oil - protein - plastic - fat - and rubber.
Volatiles
Organic chemicals
Clastic sedimentary rocks
Laccolith
2. 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.
Phreatomagmatic eruptions
Felsic - intermediate - mafic - ultramafic
Intermediate
atmospheres (atm)
3. 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.
Magnetic inclination
Sea-floor spreading
Siltstone and mudstone
Diagenesis
4. Volcanoes that exist as isolated points and appear to be independent of movement at a plate boundary - hot-spot volcanoes. Mostly are located on the interior of plates - away from boundaries.
Heat transfer
Fragmental igneous rocks
Hot spots
Biochemical sedimentary rocks
5. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Volcano
Transgression
Fissure eruptions/lava plateaus
Hydrolysis
6. 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.
Compaction
Lava
Melting
Symmetry
7. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Diagenesis
Carbonate rocks
Felsic
8. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Elemental composition of Earth
Mantle
Sea-floor spreading
Carbonate rocks
9. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
E-horizon
Hydrolysis
Marine magnetic anomaly
Hot-spot track
10. 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.
Fracture zones
Magnetic inclination
Mantle plume
Lava
11. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Chert
Lava
Sulfides
Coal
12. 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.
Igneous rocks
Transform fault
Volcanic pipes/necks
Source rock composition
13. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
The effect of the environment on eruptive style
Flood basalts
Upper mantle
Fracture zones
14. 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.
a'a'
Erosion
Area of igneous activity
Transported soil
15. 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.
Metamorphic rocks
Fumerolic mineralization
Soil Horizons
Salt wedging
16. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Magnetic anomaly
Sedimentary rocks
Continental shelf
Stoping
17. 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.
Dissolution
Quartz sandstone
Continental drift hypothesis
Columnar jointing
18. 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.
Metamorphic rocks
Convective flow
Effusive eruptions
Transition zone
19. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
3.5km (2 miles)
Conglomerate
Facets
Spreading rate
20. Low-viscosity (basaltic) lava flows out of a volcano easily - whereas high-viscosity (andesitic and rhyolitic) lava can clog and build pressure within a volcano. Basaltic eruptions are typically effusive and produce shield volcanoes - whereas rhyolit
The effect of viscosity on eruptive style
Intermediate
Tephra
Deposition
21. 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.
Paleomagnetism
Soil erosion
ravertine
Compaction
22. Type of lava flow; surface layer of the lava freezes and then breaks up due to the continued movement of lava underneath - becomes a jumble of sharp - angular fragments - yielding a rubbly flow.
Warning
: Invalid argument supplied for foreach() in
/var/www/html/basicversity.com/show_quiz.php
on line
183
23. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Metals
Fractional crystallization
Clastic sedimentary rocks
Weathering
24. 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
E-horizon
Flood basalts
Magma's speed of flow
Halides
25. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Fracture zones
Dark Silicates
Tuff
Rock texture
26. 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
Biomineralization
Crystal
Abyssal plains
Melting
27. 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.
B-horizon
Granitic composition
Symmetry
pahoehoe
28. 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.
Magnetic declination
The effect of the environment on eruptive style
Frost wedging
Assimilation
29. 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.
triple junction
Clastic
Differential weathering
Thermal expansion
30. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Dunes
Crystal habit
Tuff
Jointing
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
Dark Silicates
Silicate minerals
pahoehoe
Andesitic lava flows
32. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Zone of leaching
Rhyolitic lava flows
Chemical sedimentary rocks
Lapilli
33. Physical features of the land surface represented by changes in elevation.
Topography
Spreading rate
Granitic magma
Chemical sedimentary rocks
34. Sedimentary rock composed of calcite or dolomite.
Carbonate rocks
The effect of gas pressure on eruptive style
Ignimbrite
Magnetic inclination
35. Refers to the proportions of different chemicals making up the rock - and thus the proportion chemicals affects the proportions of different minerals constituting the rock.
Cinder cone
Cement
Rock composition
Continental drift hypothesis
36. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Sandstone
Specific gravity
Ridge-push force
Phreatomagmatic eruptions
37. The record of paleomagnetism revealed that the location of Earth's magnetic poles had been changing through geologic time. This 'wandering' meant that Earth's magnetic poles do not move with respect to fixed continents. Rather - continents move relat
The effect of gas pressure on eruptive style
Factors classifying clastic sedimentary rocks
Clastic
Apparent polar-wander path
38. 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.
Rock layering
Peridotite
Fumerolic mineralization
Outcrop
39. The way in which the atoms are packed together within a mineral by chemical bonds. Five difference types of bonding can occur - covalent - ionic - metallic - Van der Waal's - and hydrogen.
Crystal structure
Lower mantle
Glass
Fracture and cleavage
40. 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
Basalt
12km
Inner core
Granitic composition
41. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Salt wedging
Crystalline igneous rocks
Clastic
Coal
42. 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.
Columnar jointing
Inner core
Magnetic declination
Batholiths
43. The crust moves away from the Mid-Atlantic Ridge axis at a rate of 1cm per year. This velocity of sea-floor spreading is determined by the relationship between the paleomagnetic anomaly-stripe's width and the reverse polarity duration - the data reve
Spreading rate
Carbonate rocks
Felsic - intermediate - mafic - ultramafic
Fractional crystallization
44. Sedimentary rock composed of clay.
Agrillaceous rocks
Saprolite
Diagenesis
Partial melting
45. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Volcanic pipes/necks
Color
Mid-ocean ridges
Clastic
46. Molten rock beneath Earth's surface.
Magma
Alloy
Rocks
Sandstone
47. Type of magma; low in silica - fluid - crystallize at high temperatures.
Organic chemicals
Subduction
Volcanic pipes/necks
Basaltic magma
48. 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.
Conchoidal fractures
Bed
Precipitation
Oxides
49. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Alloy
pahoehoe
Upper mantle
Phreatomagmatic eruptions
50. Elongate submarine mountain ranges whose peaks lie only about 2-2.5km below sea level. Consist of a ridge axis - are roughly symmetrical - and can include escarpments - axial troughs - and valleys. Examples - Mid-Atlantic Ridge - East Pacific Rise -
Mid-ocean ridges
Dunes
Tephra
Volcano