Test #1 Study list
NEW test date Tuesday 29 April
Week 1 ( also extended into week 2)
Geography: meaning of word, what geographers study
Mental maps
Various definitions of PNW
PNW as
Shared attributes of PNW
Geologic Overview: terranes, continental glaciation, subduction, glacial till, varved clay, sands from outwash plains, deltas, meandering rivers, flood plains, levees as restricting meandering
Nisqually three questions
Regions of the PNW as per Kimerling in Ch1
Robert Thayer Reading:
Postmodern: complex term that applies to our life today, includes fragmented existences, lack of home-places, questioning of traditional authorities, globalization, can be viewed negatively or positively!
Bio-region/life-place: concept of a place with some unifying aspects
Knowledge is compartmentalized in the academic world
Biophilia – affection for living world
Topophilia as affection for land
Sustainability, or ‘sustainable development’: activities can continue and land can be passed on as productive as it was
Life-place as ‘informed by various disciplines’: knowledge and coming from different vantage points
Utopian
Carrying capacity of the land: what it can produce
Alan Thein Durning reading: Waves of resource extraction
Week 3-4 History
Alan Thein Durning reading: Waves of resource extraction
Native American relationship with the land
Manifest destiny
Extractive economies
Fur trade
Mining
Fishing
Logging
Power/irrigation/agriculture
Klondike gold rush
Alaska Yukon Pacific exhibition
Seattle: human changes to site
Tacoma & Seattle: historic and contemporary links both north and south as well as east and west
Coll-Peter Thrush paper
James Clifford paper
Week 4 Climate
Weather and climate: the difference between these two
Climate: Our
region (Puget Sound and Coastal region) - moderate climate (small range of
temperature unlike continental interior of the US
Rainfall: Unlike most of the US our maximum rainfall is in winter
Our marine west coast climate is different from a Mediterranean Climate:
cooler and wetter in winter, less hot and dry in summer: most of our
plants do not go dormant in summer.
Winter rain is available to the watertable as there
is little evaporation
Winds: Local winds: either from S
and S/W or N and N/E
Wind basics: warm air rises (think seam from kettle), but then as it rises it
condenses and cools. As air cools it can hold less moisture.
Global circulation: large
circulation cells from unequal heating of the earth (heat rises in tropics,
descends over poles) Three major
cells in the northern hemisphere. Descending air warms and therefore does
not drop moisture, descending air as cause for deserts.
Ascending air over the tropics can be seen as a band of cloud on satellite
images (cause of rain forests)
Converging air in our region along the polar front. Warm moisture-laden
air meets cooler polar air. Jet stream forms at
high altitudes above the polar front. Storms along the jet stream like
pearls on a necklace.
Additional factor that gives our region rain are the mountains: orographic
lifting.
Microclimates (within our area there
are a multitude of
microclimates, there are variations in the climate). Causes: proximity to water, N/S orientation,
tree coverage,
valleys (cold air drainage), elevation.
Local variations in rainfall: Temperature does not vary much over
Storm tracks from The N. Central US and
Also material on spits