Mountain building & the evolution of continents Chapter 20 1.Mountain belts 2.Mountain building...
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Transcript of Mountain building & the evolution of continents Chapter 20 1.Mountain belts 2.Mountain building...
![Page 1: Mountain building & the evolution of continents Chapter 20 1.Mountain belts 2.Mountain building 3.Continental accretion 4.Uplift, Basin and Range, Southern.](https://reader036.fdocuments.us/reader036/viewer/2022062421/56649d3b5503460f94a161d5/html5/thumbnails/1.jpg)
Mountain building & Mountain building & the evolution of the evolution of continentscontinents
Chapter 20Chapter 20
1. Mountain belts2. Mountain building3. Continental accretion4. Uplift, Basin and Range , Southern
Rocky mountains
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Study questionsStudy questions
What is the geologic history of the Basin and Range province and southern Rocky mountains?
What is an accreted terrane and where do they originate? What is the connection with plate tectonics?
What is the geologic history of the Himalayas and Appalachians?
![Page 3: Mountain building & the evolution of continents Chapter 20 1.Mountain belts 2.Mountain building 3.Continental accretion 4.Uplift, Basin and Range, Southern.](https://reader036.fdocuments.us/reader036/viewer/2022062421/56649d3b5503460f94a161d5/html5/thumbnails/3.jpg)
1) Mountain belts1) Mountain belts
““OrogenyOrogeny”” = mountain building = mountain building
Mountain beltsMountain belts = continuous mountain ranges= continuous mountain ranges
Huge horizontal forces in the crust build mountainsHuge horizontal forces in the crust build mountains
Signs of such forces: folding, faulting, metamorphism, Signs of such forces: folding, faulting, metamorphism, igneous activityigneous activity
Huge horizontal forces in the crust build mountainsHuge horizontal forces in the crust build mountains
Signs of such forces: folding, faulting, metamorphism, Signs of such forces: folding, faulting, metamorphism, igneous activityigneous activity
![Page 4: Mountain building & the evolution of continents Chapter 20 1.Mountain belts 2.Mountain building 3.Continental accretion 4.Uplift, Basin and Range, Southern.](https://reader036.fdocuments.us/reader036/viewer/2022062421/56649d3b5503460f94a161d5/html5/thumbnails/4.jpg)
many “young” mountain belts ( < 100 million years old)
Paleozoic and Precambrian-age mountains (> 250 millionYrs old)
mountain belts usually parallel folded/faulted ridges
sedimentary or volcanic rocks, usually intruded by igneous bodies
- Western Americas- Himalayas (45 million yrs ago)- NW Pacific, etc
- Appalachians- Urals
Fig. 20.1+19
1) Mountain belts1) Mountain belts
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2) Mountain building2) Mountain building
Convergent Boundaries
Ocean-ocean boundaries (Aleutian-type)
Ocean-continent boundaries (Andean-type)
Generates avolcanic arc
1st: a passive continental margin (like east coast of US)2nd: turns into an active margin, subduction initiates3rd: deformation, metamorphism: 2 parallel zones: accretionary wedge and volcanic arc
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2) Mountain building2) Mountain building
Subduction zones (convergent plate boundaries)
Continental collisions (examples: Himalayas, Appalachians)
Himalayas
Fig. 20.13,14,15
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2) Mountain building2) Mountain building
Subduction zones (convergent plate boundaries)
Continental collisions (examples: Himalayas, Appalachians)
Himalayas
Fig. 20.15
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2) Mountain building2) Mountain building
Subduction zonesSubduction zones (convergent plate boundaries) (convergent plate boundaries)
Continental collisionsContinental collisions
AppalachiansValley and Ridge Province in Pennsylvania
Fig. 20.4
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Formation of the AppalachiansFormation of the Appalachians
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3) Continental accretion3) Continental accretion
““Continental accretion”Continental accretion”
Small island arcs or “mini-continents”can be added to continents
Example: Western N. America
Accreted crustal blocks= terranes
Fig. 20.11Fig. 20.12
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4. Uplift, Basin and Range, Southern Rockies4. Uplift, Basin and Range, Southern Rockies
Fig. 20.5
See Fig. 20.6
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Northern Rocky Mountains, British Columbia
Deformed sedimentary rock from continental shelf deposits displaced by low angle thrust faults toward the interior of Canada.
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Fault-block mountain ranges and rift valleys
Basin and RangeBasin and Range
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Current uplift or subsidence in the U.S.Current uplift or subsidence in the U.S.
4. Uplift, Basin and Range, Southern Rockies4. Uplift, Basin and Range, Southern Rockies
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Sample MCSample MC
Where are the oldest rocks in North America located?
A. in the Appalachian MountainsB. in the Basin and Range provinceC. in the Canadian ShieldD. in the Rocky Mountains
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Sample MCSample MC
In which of the following settings were most of the rocks of the interior platform of North America deposited?
A. in a continental riftB. in a deep ocean basinC. in an extensive shallow seaD. in a volcanic island arc
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Sample MCSample MC
Why is the North American Cordillera topographically higher than the Appalachians?
A. because the Appalachians have undergone less erosionB. because the Cordillera formed by continent-continent collisionC. because the main orogeny in the Cordillera was more recentD. because the spreading rate of the East Pacific Rise is greater than the spreading rate of the Mid-Atlantic Ridge
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Sample MCSample MC
Which of the following processes is responsible for the topography of the Basin and Range province in western North America?
A. normal faultingB. strike-slip faultingC. thrust faultingD. upwarping
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Sample MCSample MC
In which of the following regions is new material currently being added to the crust?
A. Appalachian MountainsB. Canadian ShieldC. Cascade RangeD. Rocky Mountains
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Sample MCSample MC
Which of the following mountain belts formed as a result of a collision between two continents?
A. AppalachiansB. HimalayasC. UralsD. all of these
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Sample MCSample MC
What type of faults are depicted in the cross section?
A. normal faultsB. strike-slip faultsC. thrust faultsD. cannot tell from the information given
A
B
C