Physical geography Unit 3 practice questions

0.0(0)
studied byStudied by 0 people
0.0(0)
full-widthCall Kai
learnLearn
examPractice Test
spaced repetitionSpaced Repetition
heart puzzleMatch
flashcardsFlashcards
GameKnowt Play
Card Sorting

1/55

flashcard set

Earn XP

Description and Tags

from quizzes 8-10

Study Analytics
Name
Mastery
Learn
Test
Matching
Spaced

No study sessions yet.

56 Terms

1
New cards

The six major terrestrial vegetation groups discussed are forest, savanna, shrubland, grassland, desert, and tundra.

true

2
New cards

Ecotones are always abrupt.

false

3
New cards

Explain how climatic regions help predict the distribution of biomes on land. Give one example using any two biomes from the slides.

Climatic regions summarize long-term temperature and moisture patterns that control vegetation structure. Where climates are warm and wet year-round, dense forests (e.g., tropical rain forest) dominate; where climates are cold with short summers, tree growth is limited and tundra or boreal forests occur.

4
New cards

A biome is best defined as:

A large, stable terrestrial ecosystem characterized by specific plant and animal communities, often named for its dominant vegetation

5
New cards

Which statement about dry climates (permanent moisture deficits) is most accurate?

They are associated with subtropical high-pressure cells and can be extended poleward by rain shadows along mountain ranges.

6
New cards

Which group lists the core components that shape climate on Earth?

Insolation and energy balance; temperature; air pressure and winds; air masses; moisture

7
New cards

Ecosystem

Self-sustaining association of organisms and their abiotic environment

8
New cards

Biogeography

Study of the distribution of plants and animals

9
New cards

Biome

Large, stable terrestrial ecosystem named for dominant vegetation

10
New cards

Ecotone

Boundary zone between adjoining ecosystems

11
New cards

Which of the following pairs correctly matches a climate classification approach with what it uses?

Genetic → causative factors (e.g., circulation, energy balance); Empirical → statistical temperature and precipitation data

12
New cards

Mesothermal climates (mild winters)

Midlatitudes with migrating cyclones; strong land–sea contrasts

13
New cards

Polar and highland climates

Low sun angles, long winters, low humidity; Earth’s frozen deserts

14
New cards

Microthermal climates (cold winters)

Continental interiors with cold winters; strong air-mass contrasts

15
New cards

Tropical climates

Consistently warm; seasonal rains migrate with the intertropical convergence zone

16
New cards

Deserts occupy less than 10% of Earth’s land surface.

false

17
New cards

What primary evidence reveals Earth’s internal structure?

Seismic waves from earthquakes

18
New cards

The base of the crust is marked by which boundary

Mohorovičić (Moho) discontinuity

19
New cards

What generates Earth's magnetic field?

Movement of liquid metallic outer core

20
New cards

Large mineral crystals in an igneous rock most directly indicate:

Slow cooling underground (intrusive)

21
New cards

The asthenosphere is the rigid layer (crust plus uppermost mantle) that forms tectonic plates; the lithosphere below is weak and plastic

false

22
New cards

The principle of superposition states that in an undisturbed sequence of layered rocks, the youngest layer is at the top.

true

23
New cards

In the oceans, the oldest rocks are found at the mid-ocean ridges.

false 

24
New cards

Gutenberg Discontinuity

Boundary between outer core and mantle

25
New cards

Asthenosphere

Weak, plastic zone of the upper mantle below the lithosphere

26
New cards

Lithosphere

Rigid outer shell made of crust plus uppermost mantle (tectonic plates)

27
New cards

Moho discontinuity

Boundary between crust and mantle

28
New cards

Mineral

Natural, inorganic substance with a specific chemical formula and crystalline structure

29
New cards

Sedimentary rock

Forms by lithification of fragments or chemical precipitation

30
New cards

Metamorphic rock

Forms when pre-existing rock changes by heat and/or pressure

31
New cards

Igneous rock

Forms by cooling and solidification of molten material

32
New cards

Radiometric dating

Determining numerical ages by measuring parent and daughter isotopes

33
New cards

Superposition

In undisturbed layered rocks, the oldest is at the base and the youngest at the top

34
New cards

Uniformitarianism

The present is the key to the past; the same physical processes operated in the past

35
New cards

Give two independent lines of evidence that support plate tectonics, and explain in one sentence each how they support the theory.

Two pieces of evidence for plate tectonics is the fact that fossils are similar all over the world, and that all of the contents fit together. If all of the continets are looked at, you can see that they all look as if they should fit together as if a puzzle. for fossil evidence, you can see that the land animals who do not swim, can be found in different, non connected continents, proving that all of the continents were once connected.

36
New cards

Briefly describe the rock cycle by explaining how one rock type can transform into each of the other two.

Igneous rock weathers to sediments that lithify into sedimentary rock; sedimentary or igneous rock can be altered by heat and pressure to become metamorphic rock; any rock can melt to form magma that cools into new igneous rock

37
New cards

Which data set most directly outlines tectonic plate boundaries on a global map?

Earthquake locations and volcanoes

38
New cards

Which combination best characterizes ocean–continent convergence?

Deep trench, volcanic mountains on the continent, and deep earthquakes (to ~600 km)

39
New cards

Which statement best describes transform plate boundaries?

Plates slide past; surface features offset laterally; shallow earthquakes are common

40
New cards

What features are typical of continental collision?

Thickened lithosphere, tallest mountain ranges, rare volcanism

41
New cards

The elastic rebound theory explains that rock elastically deforms as stress builds and then snaps to a new position when the fault slips, producing an earthquake.

true

42
New cards

The Richter scale is used worldwide and has fully replaced the Moment Magnitude scale for measuring earthquake size.

false 

43
New cards

Hot spots move laterally through the mantle, producing straight volcanic chains while plates stay fixed.

false

44
New cards

Compression

Shortening with folding and thrust faults

45
New cards

Tension

Stretching with normal faults and rifting

46
New cards

Shearing

Lateral motion with transform faults

47
New cards

Caldera

Basin-shaped summit collapse ≥1 km after major eruption

48
New cards

Stratovolcano

Large, layered lava/ash; high-viscosity magma; explosive

49
New cards

Shield Volcano

Broad, low profile from many basalt flows; effusive

50
New cards

Cinder Cone

Small, scoria-rich cone; often in clusters

51
New cards

S-wave

Up–down shear motion (body wave); second fastest

52
New cards

Rayleigh Wave

Retrograde rolling motion like a backward ocean wave (surface wave)

53
New cards

P-wave

Compressional motion; fastest body wave

54
New cards

Love Wave

Side-to-side “snake-like” surface motion

55
New cards

Describe the relationship between volcanic eruptions (explosive, effusive) and magma temperature, gas content, and silica content.

The viscosity and gas content will determine the type of eruption in a volcano. Higher temperatures and lower silica content will make magma less viscous, therefore leading to an effusive eruption. Lower temperatures and high silica content will make the magma more viscous, + high gas content will make magma explosive.

56
New cards

Describe how continents grow through terrane accretion.

Continents grow when buoyant crustal fragments—such as microcontinents, island arcs, oceanic plateaus, and sediment packages—arrive at a subduction margin on an oceanic plate and are too light to sink; they get scraped off and welded onto the continental edge, creating accretionary wedges and suture zones. Repeated docking of these terranes thickens the crust and builds mountain belts.