Midterm & Glaciers Flashcards

(138 cards)

1
Q

Relative Time

A

Determines the sequence of events

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2
Q

Absolute Time

A

Determines the date/age of events

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3
Q

Geologic Principles

A
  1. Original Horizontality
  2. Superposition
  3. Inclusions
  4. Cross-cutting relations
  5. Contact margins
  6. Faunal succession
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4
Q

Original Horizontality

A

Rock is initially laid down horizontally; any change in angle has been cause afterwards

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5
Q

Superposition

A

Rocks that are closer to the surface are younger

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6
Q

Inclusions

A

Young rock can contain pieces of older rock

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7
Q

Cross-cutting relations

A

Young rock or features can cut across older rock or features

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8
Q

Contact Margins

A

A young rock/feature can cause changes along the contact line with an older rock/feature

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9
Q

Faunal succession

A

Fossil assemblages can be correlated to specific deposits/time periods

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10
Q

Unconformities

A

Periods of time that are missing from the geologic record

Still help us determine what happened during that time; we know that there was uplift, erosion, etc.

Three types:

  • Angular unconformity
  • Nonconformity
  • Disconformity
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11
Q

Angular unconformity

A

rock is uplifted, eroded, then new sediment is laid horizontally on top

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12
Q

Nonconformity

A

Sedimentary rocks overlie intrusive igneous rocks and/or metamorphic rocks

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13
Q

Disconformity

A

Contact between two beds represents a period during which no deposition occurred - i.e. there is a large gap in the age of the two sediments

So basically they’re like that 51-year-old and 16-year-old getting together

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14
Q

Radiometric dating

A

Radioactive isotopes decay randomly but at a set rat, meaning we can predict how long it takes for them to decay to a certain ratio of daughter and parent isotopes

Assumes that there has been no loss or gain of parent or daughter isotopes, and the rock is below closure temperature (and has been since it was formed)

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15
Q

Body fossils

A

The actual physical remains of an organism (i.e. skeleton) has been left behind and mineralized

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16
Q

Trace fossils

A

Evidence of an organism’s existence in an area has been preserved in the rock (i.e. footprints, coprolite)

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17
Q

Concordia Curve

A

Plotting two things against each other (ex. two half-lifes) to form a curve, then plotting experimental data along the same plot to see if they come up with a similar answer

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18
Q

Fission tracks

A

Disintegration of the nucleus of 238U create sausage-shaped tracks within a mineral

You can determine age by counting tracks

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19
Q

Rhythmic processes

A

Can be used as absolute dating methods, e.g:

  • Varves (yearly patterns in lake sediment deposition)
  • Corals (daily growth marks)
  • Magnetostratigraphy (reversals of earth’s magnetic field)
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20
Q

Geologic Timescale

A

Division of earth’s history into eons, eras, periods, and epochs

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21
Q

Eons

A

Largest division of time on the geologic timescale:

  • Hadean
  • Archean
  • Proterozoic
  • Phanerozoic
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22
Q

Eras

A
  • Palaeozoic
  • Mesozoic
  • Cenozoic
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23
Q

Oldest Rock

A

Acasta gneiss from the Northwest Territories

4,025 +/- 15 Ma

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24
Q

Age of the Earth

A

4.567 Ga

Determined from the age of meteorites believed to be from the same time the solar system was formed

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25
Oldest mineral
Zircon in Australian rock 4.3 Ga
26
Uniformitarianism
The present is the key to the past The processes that worked in the past are the same as the ones that are observable today, so we can infer what happened in the past from our knowledge of the present
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Igneous Rocks | Geologic History
Signs of intrusions and eruptions of magma
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Sedimentary Rocks | Geologic History
Record environmental changes - Mode of transport and environment of deposition i.e. Climate, life, sea level
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Metamorphic Rocks
Record collisions of plates, uplift and erosion of mountains
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Cenozoic
Age of mammals and flowering plants 65 Ma - present
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Mesozoic
``` Age of dinosaurs - Development of bipedal movement First birds First mammals First angiosperms ``` 251 - 65 Ma
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Palaeozoic
Cambrian explosion - beginning of the fossil record Life conquers land: plants, lungs, reptilian eggs - All animals are reptilian or amphibious 542 - 251 Ma
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Phanerozoic
Encompasses the time of Earth's history with a lot of diversification of life: "visible life" 542 Ma - Present Palaeozoic, Mesozoic, Cenozoic
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Proterozoic
Photosynthesis puts oxygen into the air First eukaryotic cells 2,500 Ma - 542 Ma
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Archean
Earth first becomes habitable First continental crust First life 3,800 Ma - 2,500 Ma
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Hadean
Earth's early life Inhabitable 4,567 Ma - 3,800 Ma
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Sedimentary rock coverage
Sedimentary rock makes up a very small portion of the rock on the earth's surface, but it is still very important because it holds important clues about earth's history
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Weathering
Two types: physical and chemical They work in conjunction with one another
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Physical weathering
Weathering of a rock that results in smaller pieces of the rock - Jointing - Thermal expansion - Wedging by frost, roots, salt - Burrowing
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Chemical weathering
Weathering of rock that results in ions that can be moved away - Dissolution (ex. salt, limestone) - Hydrolysis (ex. feldspar --> clay) - Oxidation (ex. biotite/pyrite --> hematite) - Hydration (ex. clays)
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Sediment sizing
``` Boulder: > 256mm Cobble: > 64mm Pebbles: > 2 mm Sand: > 1/16 mm Silt: > 1/256 mm Mud ```
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Soil
A mixture of mineral fragments, water, air, and organic matter Bedrock breaks down into regolith, which then mixes with organic matter to create humus
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Regolith
Small rock particles that have the potential to become, but are not yet, soil
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Humus
Soil that is able to support life
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Soil horizons
``` Zone of leaching - - Topsoil (O & A1) - Transition (A2) Zone of accumulation - Subsoil (B) Bedrock (C) ```
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Desert soil
Thin Occasionally has hard salt/calcite crust
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Tropical soil
Thick laterite soil, but very nutrient deprived | - No B horizon, but Al-rich A2
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Clastic sedimentary rocks
The products of physical weathering Described based on size, composition, roundness, sorting of clasts, and cement type (quartz or calcite) E.g. - Conglomerate/breccia - Sandstone/arkose - Siltstone - Mudstone/shale
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Sediment maturity
As sediment moves farther from the source, it gets more "mature" - more spherical, better sorted, higher proportion of resilient minerals
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Chemical sedimentary rocks
Rocks that are formed from chemical precipitation E.g. - Evaporites (rock salt/gypsum, saltwater evaporation) - Tavertine (chemical limestone) - Banded iron formation: very old
51
Biochemical sedimentary rocks
Rock formed from the remains of prehistoric organisms - Limestone (calcite shells) - Chert (shells of plankton like radiolaria, diatoms) - Coal (plant debris)
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Bed
Has a recognizable bottom and top Generally relate to one depositional event
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Contact
Surface that separates two beds | Can be gradational or abrupt
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Lateral contacts
Contacts between beds that are beside one another Can be: - Pinched out - Interfingering - Gradational
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Strata
A series of beds
56
Formation
A distinctive (and mappable) series of strata Often named based on the place it was discovered and the rock type (e.g. Toronto Limestone)
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Conformable strata
Laid down with no interruption
58
Hiatus
A break in the geologic record
59
Bioturbation
Disturbance of rock caused by burrowing animals (ex. worms, clams)
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Ripples and dunes
Deposition within a current of water or wind Results in cross-bedding
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Graded bedding
Beds within which the coarsest sediment was deposited first and the finest sediment last Happens in turbid water
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Load casts
Impressions made on the base of a bed where a dense sediment (sand/pebbles/boulders) overlaid a much softer sediment (mud/silt)
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Flute marks
Scours dug into the top part of a bed get filled in by later strata, taking a cast of the scour marks
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Sedimentary environments
Terrestrial: - Rivers - Lakes - Glacial - Sedimentary basins Marine - Deltas - Beaches - Shallow water - Carbonate reef - Deep ocean
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Facies Concept
Distinct sedimentary characteristics reflect distinct processes Our knowledge of present-day sedimentary environments can allow us to reconstruct palaeoenvironments from sedimentary rocks
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Hydrological cycle
The cycle of where water is stored and where/how it moves
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Earth's water
Freshwater accounts for only 3.5% of earth's water Of this freshwater, only 0.3% is surface water - the majority is ice cap/glacier and groundwater Of surface water, most is contained in lakes
68
Human use of freshwater
1. Irrigation (39.6%) 2. Thermoelectric Power (39.3%) 3. Public and Domestic Use (13.5%) 4. Industrial Use (5.3%) 5. Aquaculture (1.1%) 6. Mining (0.6%) 7. Livestock (0.5%)
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Drainage Basin
A drainage network that collects water from a broad region AKA watershed
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Drainage divide
The highland or ridge that separates one watershed from another
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Drainage patterns
The patterns that water tends to follow when draining from a source into the basin - Dentritic - Radial - Structurally controlled
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Dentritic drainage
Resemble the branches on a tree Form on a land with uniform substrate
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Radial drainage
Water drains radially from a centre point Generally happens when the source is the high point of a conical mountain
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Structurally controlled drainage
Water follows the path of the well-defined topography underneath I.e. through joints, along valleys
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Equilibrium Profile
Measures the elevation, sediment load, water load, or water velocity of a river against the distance from its source
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River erosion
Occurs through scouring, breaking, lifting, abrasion, and dissolution Depends on discharge and sediment content
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Braided River
Looks like the intertwining hairs in a braid - Large volume of bedload - Banks erode very easily - Shifting bars
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Meandering River
Looks like a snake winding across the landscape - Mostly suspended load - Cohesive banks - Cutbanks, point bars, oxbow lakes - Erosion takes place on the outer edges of meanders
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Point bar
The area of sediment deposition on the inside of the meanders of a river
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Oxbow lake
Lakes that have been formed when a meander of a river cuts in so close that it cuts itself off
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Suspended load
Sediment carried within the body of a river; smaller particles that the water is able to float along with it
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Bedload
Sediment that is dragged, bounced, or rolled along the bed of a stream; larger particles that can only be moved by a large amount of force
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Dissolved load
Ions that are dissolved in the stream and carried along with it
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Mountain streams
Typically form steep V-shaped valleys
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Terrace
River downcuts into the ground, leaving a "terrace" of raised ground surrounding its floodplain
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Rapids
Particularly turbulent water with a rough surface; forms when: - Water flows over steps or large clasts in the channel floor - Channel abruptly narrows - Gradient abruptly changes
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Waterfall
Forms where the gradient of a stream becomes so steep the water free-falls down the stream bed
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Alluvial fan
Gently sloping apron of sediment Forms when a fast-moving stream abruptly emerges from a confined space and spreads out, slowing down and quickly dropping its sediment load
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Levee
Accumulation of sediment in a pair of low ridges on either side of a stream
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Flood
When the volume of water flowing exceeds the capacity of the stream channel and flows over into the floodplain areas on either side of the stream
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Shallow-marine sediments
Gradient deposition, with larger clasts deposited closer to shore and finer clasts further out; clasts are well-sorted and rounded Contain marine fossils and tend to become siltstone/mudstone
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Tropical marine sediments
Shallow marine environments that contain a large amount of carbonate shell debris Indicate the presence of a reef
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River sediments
Fine sediments are deposited along the shores Sediment ripples due to being deposited within a current - cross bedding Sandstone, siltstone, shale
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Delta sediments
Present as thick sequences where deeper-water sediments slowly grade into river sediments
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Saturated zone
Area of groundwater where all pores are filled with water - no air
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Water table
Line that separates the saturated zone of groundwater from the unsaturated zone
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Vadose zone
Area above the water table where water partially fills the pores in the ground but not fully
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Porosity
Actual amount of space there is in between particles that can be filled by water
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Permeability
Connectivity between pores - allows water to flow within a substance
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Groundwater flow
Will always flow from high to low hydraulic head
101
Hydraulic head
Potential energy available to drive the flow of a given volume of groundwater at a location
102
Aquifer
Sediment rocks that transmit water easily Provides water to wells
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Aquitard
Sediment/rock that does not transmit water easily and therefore slows it down
104
Cone of depression
When water is pumped out a well too quickly and the water table sinks down around the well, forming a pointed-down cone shape
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Karst
A network of underground caves that have been carved out of limestone by water Collapse of these caves causes a landscape of sinkholes or limestone spires
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Sinkhole
Circular depression in the ground that happens when an underground cave collapses
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Speleothems
Formations that grow in caves from the accumulation of dripstone Stalactite: hangs from the ceiling Stalagmite: emerges from the ground Limestone column: happens when a stalactite and stalagmite merge
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Disappearing Stream
Where a surface stream enters into a crack or hole and travels for some time in underground caves
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Spreading of contaminants (groundwater)
Contaminants can enter the groundwater and then travel within the water, potentially ending up in well water
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Map scales
Expressed as a ratio (e.g. 1:500,000) Means that one unit measured on the map is equal to 500,000 units on the ground - 1 cm = 500,000cms or 5km in reality
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Topographic contour lines
Connect all points of equal height above a certain datum (usually sea level)
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Contour interval
Height difference between two subsequent contour lines
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Cross-section
Represents the topography and geological structures on a specific line across the earth
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UTM
Universe Transverse Mercator Uses Northing and Easting instead of Latitude and Longitude
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Northing
Distance to the equator (km)
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Easting
Measured to a central meridian (degrees)
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Azimuth
Position on a sphere measured in degrees For true-north, north is 0%, south is 180%
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Zone of Accumulation
Area of glacier where ice accumulates and begins to flow downhill
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Zone of Wastage
Area of glacier where ice melts and begins to recede AKA zone of ablation
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Glacier advance/retreat
Advances if accumulation > wastage | Retreats if accumulation < wastage
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Valley glacier
Basically a river of ice flows down a mountain side into a valley
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Moraines
Pile of debris deposited by a glacier Lateral moraines: Formed along the edges Medial moraines: Formed where two glaciers meet, run in the middle of the composite Terminal moraines: Formed at the toe of the glacier
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Glacial valleys
U-shaped Formed because the glacial abrasion/plucking both lower the floor of the valley and bevel its sides
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Arretes
Residual edge of a rock that resembles the edge of a knife Pointy edge of the mountainous region surrounding the valley
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Roche moutonee
Glacially eroded hill, elongate in direction of flow - Upstream part = gentle slope (rasping) - Downstream edge = steep slope (plucking)
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Esker
Snake-like ridges of sand and gravel that form when sediment fills meltwater tunnels at the base of a glacier
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Drumlin
Streamlined, elongate hills that have been molded by the flow of a glacier
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Glacial Striations
Long gouges, grooves, or scratches within the bedrock over which a glacier passes - Caused by rasping of large clasts that are being carried along with the glacier
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Erratic
A boulder or cobble that was picked up by a glacier and deposited hundred of kilometres away from the outcrop from which it detached
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Till
A mixture of unsorted sediment deposited by glaciers
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Greenhouse effect
Trapping of solar heat inside the Earth's atmosphere by carbon dioxide and other greenhouse gasses that absorb infrared radiation Changes the average temperature on earth from -19 to +15 degrees Celsius
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Climate Forcing
Caused by: - Greenhouse effect - Variation in earth's orbit/tilt/precession - Thermohaline circulation - Albedo
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Eccentricity
Over the coure of 100,000 years, earth's orbit will change from more eccentric (more oval) to less eccentric (more circular) Changes the length of seasons and variability in temperature
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Tilt
Over a period of 41,000 years, the tilt of earth's rotational axis changes from 22.1° and 24.5° and back again Changes the variability in temperature across the planet - more variability with more tilt
135
Precession
Over 23,000 years, the north pole changes from pointing to the North Star to Vega
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Thermohaline circulation
The rising and sinking of water within the oceans, driven by differences in water density - Change in density due to differences in temperature and salinity (colder/more saline = denser) Circulation involves both surface and deep-water ocean currents - Water in polar areas sinks and flows along the bottom of the ocean toward the equator Prevention of thermohaline circulation shuts down the Gulf Stream
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Albedo
The reflectivity of a surface - Ice is highly reflective, so lots of ice = less heat absorbed Increasing albedo causes cooling, decreasing albedo causes warming
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Climate Change in Earth's History
Today, temperature is fairly cold in comparison to how it has been in the past - There have been multiple ice ages in the past We can also record past CO2 levels from ice cores taken from the Antarctic