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History of Oregon - Physical Geography Flashcards | StudBud
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History of Oregon - Physical Geography
History of Oregon - Physical Geography
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1
This geographic region was formed by basalt eruptions and post-Ice Age catastrophic flooding
the Puget-Willamette Lowland
The Oregon Coast
The Columbia Plateau
The Central Oregon Plateau
2
This is/These are considered the "water bank" of eastern Oregon
The Cascades
The Snake River
The Blue Mountains
The Columbia River
3
The Oregon Coast, Coast Ranges, and the Willamette River Valley share a ___ climate
Shrub Steppe
Mediterranean
Marine West Coast
High Desert
4
Are you going to die?
Everybody dies. Not everybody lives.
YES!! PANIC NOW!!!
No. I'm immortal.
What's for lunch?
5
There is a three-in-ten chance there will be a major (8.0+) eruption along this fault in the next 50 years.
Cascadia Subduction Zone
The Olympic-Wallowa Linement
The San Andreas Fault
The Juan de Fuca Fault
6
East of the Cascade Range, impacts from a Cascadia quake could include all of these
EXCEPT
power and cell phone outages
refugees from western Oregon
a tsunami
fuel shortages
7
Apart from the Cascade Range, tall mountain peaks can be found in
the Coast Range.
the Columbia Plateau.
the Blue and Wallowa Mountains.
Basin and Range.
8
These types of building are particularly vulnerable to damage from an earthquake
Hospitals
Wood frame homes
Unreinforced Masonry Buildings
Bridges
9
The Umatilla River empties into the Columbia River, making the Umatilla River
a second-order tributary.
a first-order tributary.
smaller.
a mainstem river.
10
The Columbia River begins in ___ and empties into the Pacific Ocean at Astoria.
Washington
The Snake River
The Pacific Ocean
Canada
11
This geographic region of Oregon is the state's driest and continues through nearly all of Nevada.
Basin and Range
The Coast Ranges
The Central Oregon Plateau
The Columbia Plateau
12
This geographic region gets its elevation from an ocean plate sliding beneath it.
The Coast Ranges
Basin and Range
The Cascade Range
the Blue Mountains
13
Because of accretion, the Cascadia Subduction Zone mechanism is slowly moving
south
north
west
east
14
Studies suggest that lives could be saved during a Cascadia earthquake by
building public buildings in ground high enough to escape a tsunami.
seismically retrofit buildings, bridges, and other structures.
Use bracing and anchor plates on unreinforced masonry buildings
All of the above
15
Base Isolation can
keep structures built on sandy soils from collapsing.
lead to lonliness, alienation, and the writing of bad poetry.
keep structures from shaking violently enough to be damaged.
protect against lightning strikes.
16
An ocean plate sliding beneath a continental plate is an example of
A transform fault
Spreading
Subduction
Accretion
17
The decreasing moisture content in the air after traveling over mountains is called
the Cariolis Effect
the Rain Shadow Effect
the Plains Effect
the Marine West Clast Climate
18
This Oregon river is
NOT
a part ofthe Columbia River Drainage
Snake
Rogue
Grande Ronde
Willamette
19
The number of water pipes that could be ruptured in Portland by a Cascadia quake
1,000
300
3,000
1,599
20
Cascade peaks are fed by magma that used to be part of the Juan de Fuca plate, Therefore, these peaks are
removing moisture from the air.
active volcanos.
unable to grow trees above a certain elevation.
really tall.