Exam II chapter 5 &6

Matter, Energy, Information to a system
External Costs
Pollution and waste during an item’s production
Stream Gradient
Measure of Stream channel elevation change
Abiotic inputs for rotting log ecosystem
rainfall, temperature, sunlight
Transition zone between adjacent ecosystems
Debris Apron
Transition zone between rotting log and soil
Included in environmental impact statement
Needs for project, alternatives, enc. effects
Setting for most productive ecosystems
Humid, Tropical to sub tropical
Values of a Cherokee Talking Tree
Scientific, Cultural, Educational
Processes occurring within a system
Coca Cola principle
Cold water can store more carbon dioxide gas
Favor prudent use of natural resources
Negative feedback loop
Processes that slow down a system
Abiotic stream imputs
Temperature, dissolved oxygen, pH
Edge Effect
Forest changes due to low angle sunlit margin
Natural Methods of ecosystem recovery
Seed transport by wind or animals, fire cleansing
Ways that we affect the water cycle
Cutting down forests and building dams
Full cost pricing
Internal and external costs of a consumer item
Positive feedback loops
Processes that speed up a system
Primary Succession
Ecosystem recovery after a major change
Downsides of reusable beverage bottles
Shipping to bottler, washing, greater weight
Littoral ecosystem
Shallow, self like lake ecosystem with plants
Conditions favorable to limestone deposition
Warm shallow well sunlit sea water
Secondary Successon
Ecosystem recovery after minor changes
Orographic Effect
Uplift of Air Masses by Mountains
Rain Shadow Effect
Mountains block passages of rain casting a “shadow” of dryness behind them
Plate Tectonics
is called a Unifying Theory because it explains the locations of most volcanoes & earthquakes, as well as the locations & shapes of continents & the distribution of fossils and mineral resources.
Convergent Zone
Same as “subduction”denser oceanic crust sinks into mantle beneath other plate margin. Sinking plate melts to form magma. Rising magma = volcanoes.

Divergent Zone
rising man-tle plume causes plates to separate, spread. Mid-Atlantic Ridge. Same as rift
Transform Zone
Plates slide past one another. Plate movement = earthquakes (San Andrea Fault)
Post WWII seafloor mapping used
sonar & magnetometers. Seafloor ridges & trenches, coupled with seismic data from earthquakes, and other data helped “close the loop” and explain how it happened.

Alfred Wegener (1915)
suggested the name Pangea for the supercontinent that broke apart to form the present day continents.
Oceanic Crust
More dense than continental crust but thinner. Fe-rich.
Continental Crust
lighter, Qtz-rich, light colored.

Makes up 70% of earths crust

Mafic Composition
silicate mineral or rock that is rich in magnesium and iron. example: Basalts
Felsic Composition
a term used in geology to refer to silicate minerals, magma, and rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium
Continental Rift Zones
A long, narrow fissure in the Earth marking a zone of the lithosphere that has become thinner due to extensional forces associated with plate tectonics.
Cascade Mountains
The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains (Mount Renier, Mount St. Helen)
Continental Arc System
Cascade Mountains exist because of an offshore subduction zone.
Island Arc System
is a type of archipelago composed of a chain of volcanoes which alignment is arc-shaped, and which are situated parallel and close to a boundary between two converging tectonic plates.
Western margin
Active margin
Eastern margin
Passive margin
solidified from molten rock
hardened sediments, derived from weathering and erosion of older rocks
rocks that have changed due to heat and pressure
Intermediate rock
from tall, conical composite volcanoes. Inland from Subduction Zones. Medium-colored, explosive pyroclastic ash eruptions and thick lava flows.

Erupted from caldera type.
Shield Volcano
a type of volcano usually built almost entirely of fluid lava flows. They are named for their large size and low profile, resembling a warrior’s shield.
Diabase in shallow intrusion, Norcross, GA
Youngest igneous rocks in ga
Crater Lake
After Mt. Mazama magma chamber emptied (7,000 yrs ago), the peak collapsed in on itself, resulting in the caldera, which was filled by rain and snow.
Breaking down of rock material.

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Chemical and physical

is the down-gradient transport of degraded rock (sand, gravel, clay) by way of streams & rivers to eventual deposition in the ocean.
Bedrock turns into saphrolite
Over time, with Physical and Chemical Weathering, the biotite gneiss becomes the saprolite
the drop in feet/mile. Steeper gradient = higher stream energy (velocity) and more vertical erosion of channel (downcutting) and less lateral erosion, leading to “V-shaped” valleys in mountains.
“Youthful” Streams
Mountain stream environment High energy, high oxygen content, low temperature= low biodiversity.

Meandering river
A meander in general is a bend in a sinuous watercourse. A meander is formed when the moving water in a stream erodes the outer banks and widens its valley
Most sedimentary rocks were
deposited in shallow marine conditions
Transitional environments
beaches, tidal flats
are stretches along the coast that have been exposed by the sea due to a relative fall in sea levels. This occurs due to either isostacy or eustacy.
are stretches along the coast that have been inundated by the sea due to a relative rise in sea levels. This occurs due to either isostacy or eustacy.
Rocky Shore
an intertidal area of seacoasts where solid rock predominates.
Sandy Shore
also called beaches, are coastal shorelines where sand accumulates.

East shore
Emergent shoreline. Sandy shore habitat
West Shore
Submergent, rocky shore habitat
found in deeper and/or quieter water where shales are deposited
Aquatic ecosystem
ecosystems largely controlled by water depth, water energy, clarity.
close and often long-term interaction between different biological species.
is the way two organisms biologically interact where each individual derives a fitness benefit.
When corals are stressed they
bleach and expel the algae