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Set of geomorphic features subject to similar combination or set of exogenic processes |
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geographically delimited coastal region may contain cliffs, bays, beaches defined by closed system of sediment supply and distribution length of a coastal area |
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coastal area perpindicular to the shore |
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furthest extent of wave or tidal influence |
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the depth beyond capacity of waves to deposit sediment |
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fluctuating point of contact with water |
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zone of interaction between shallow and deeper water |
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deposition of sediment seaward of surfzone - resupply of beach |
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slightly elevated areas of beach that indicate waterline |
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above the normal tidal range but can be affected by storm surge |
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refracted waves strike the coast at oblique angles, from the side, and create a horizontal current in and seaward of the surf zone |
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effect of longshore current - transport of beach sediment along the LZ horizontally |
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movement of sediment along the beach within the swash zone travels in same direction as longshore current |
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gentle wave action period of higher deposition of shore berm formation above high tide level steep beach face |
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stronger waves - period of high erosion deposition offshore - sandbars - submerged beach sediment |
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created by wind blown beach sediment in motion limited by stabilizing effects of vegetation |
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undulations in a body of water caused by friction of wind on the surface primarily generated by storms at sea but also earthquakes and landslides - seismic sea wave |
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series of swells - can travel thousands of KM |
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open water waves water particles move in circular motion horizontal movement of wave energy transference of energy through water - not trans of water |
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shallow water waves - approach to shore decrease in depth = increase in frictional drag wavelength decreases - closer together |
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oncoming waves slow down at coastal approach conform to submarine topography -> bending of wave train (refraction) concentration of wave energy at areas of resistance |
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convergence of wave energy |
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at coastal protrusions erosional |
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divergence of wave energy |
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Definition
in bays and coves depositional |
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hydraulic action - force of moving water - augmented by wave energy dislodging of particles and rock EX: sea stacks, sea arches, sea cliffs |
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suspended sediments scour rocks |
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suspended load is deposited when wave energy dissipates in the swash zone EX: beach - deposit of coastal sediment and material of various sizes |
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continuous - ocean beach SF |
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consists of pebbles, rocks and stones derived fro local, resistant rock |
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broken up pieces of coral, shells and exoskeletons of sea creatures - bioclasts typical of tropic and subtropic communities - closer to coral reefs |
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weathered and eroded pieces of igneous extrusive rock further disintegrated by wave action |
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rapid, dramatic increase in wave height |
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seismic sea wave as high as 20m |
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to determine potential extent of coastal submergence |
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wind as agent of erosion and transportation wind behaves like a fluid but with low viscosity smaller capacity to erode and transport compared to water and ice |
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two principle processes of eolian erosion |
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1. deflation: removal lifting and scattering of loose particles 2. abrasion: air born particles erode surfaces by scraping and sculpting "sandblasting" |
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bouncing and skipping of particles |
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impact of saltating material dislodges and moves other particles |
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fine particles transported by suspension and deposited into thick, cohesive beds |
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particles become airborne |
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crescent shaped strong prevailing wind from one direction |
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continuous ridges moderate prevailing wind - little variation in direction abundant sand supply typical beach dunes |
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ridge shaped - paralled to prevailing wind strong winds from two directions abundant sand supply |
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wind sculpted linear rock formation formed by deflation and abrasion aligned parallel to effective wind |
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removal of loose particles and transport by suspension |
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scouring of material by airborne particles |
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zones of subtropical high pressure |
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descending warm, dry ait masses at 23-30 N/S |
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effect of mountain ranges of leeward areas - dry climates |
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long distance from large bodies of water |
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shaped by eolian and fluvial processes - ephemeral streams/stream channels subject to rapid high flow during rain events - flash flood |
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stream transition from steep to low gradient spread of alluvium in all directions cone distributed sediment at canyon mouth successive build up from ephemeral/seasonal flow |
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mass of ide formed by thickening and compaction of snow and water over time minimum of 40 m thick |
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alpine glaciers (mountain glacier) |
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result of cold conditions at high elevation usually form in valleys located worldwide |
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located in polar and near polar latitudes thick and extensive greenland and antarctica |
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any glacial mass that covers an entire landscape |
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granual snow in transition to ice survives seasonal melting indicates extent of glacial accumulation |
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accumulates based of glacial year each layer indicated one season of accumulation |
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"river of ice" pliable plastic consistency more pliable at base and brittle on top motion by basal slip |
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velocity profile of glacial flow |
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Definition
flow at surface is greater at base - creates crevasses |
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dislodging and picking up material from weight of glacial mass |
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from weight of ice and abrasion |
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scouring of landscape from material embedded in the glacier |
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bowl shaped head of glacial valley |
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flows into the main glacier |
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lateral glacier fractures |
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rock and sediment debris transported by glacial advance - deposited as ridges or hills |
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till deposits between glaciers |
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sits above glacial through - formerly terminated at main glacier |
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carved by glaciers at base |
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glacial valley inundated by seawater |
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ridge or crest that indicates furthest point of glacial advance |
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area of braided streams, lakes, ponds and depressions at glacial edge |
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ridge of glacial till - unsorted clasts of all sizes |
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rocks and boulders left behind during glacial retract |
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cover a significant portion of a large land mass minimum of 50000 sq/km |
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Quaternary period Pleistocene Epoch Ice age |
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Definition
1.8-2 million years ago begins defined by a sequence of alternating glacial and interglacial periods in 100,000 year cycles advance and retreat of continental ice sheets and alpice glaciation in Northern latitudes |
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Ice age positive feedback loop |
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Definition
more ice cover: more snowfall / ice cover higher albedo reduces summer melting |
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How was the world different during last Glacial Maximum? |
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Definition
colder: 4-9 C lower than today drier: expansion of grassland, savannah and semi arid compaction of forests less circulating moisture - trapped in ice sheets |
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Definition
realm of all living things - atmosphere, lithosphere, hydrosphere ocean floor, underneath the ground to altitudes 8km |
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study of spatial distribution of flora and fauna and the processes that produce these spatial patterns |
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community of organisms functioning together in an interdependent relation with the environment they occupy |
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no living components/factors |
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biotic subdivision of an ecosystem |
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large terrestrial ecosystem consisting of numerous smaller, related subsystems like ecosystem and community |
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spatial extent of a habitation by a particular species (ecosystem is a collection of habitats) |
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combination of role or function of a particular species and its habitat what it does and where it does it |
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area of transition between ecosystems can be abrupt or gradual |
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plant life - primary producers primary biotic component of most terrestrial systems convert solar energy, water, C02 into carbohydrates (photosynthesis) |
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global net primary productivity (NPP) |
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rate at which new, primary organic material is created measured in organic carbon (grams)/sq meter |
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more green in spring only green in S hemisphere in winter more green in N hemisphere in summer more green in Southern hemisphere in Fall |
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decomposers - begin process of rot detrius eaters consume waste and release nutrients back to soil |
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similar abiotic conditions produce related biotic systems |
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temperature/precipitation of eco. |
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warm and wet conditions produce dense and diverse systems cold and dry produce sparse systems moisture is the controling factor independent of temperature |
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factor in climate regime - ecosystem type |
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distribution of biome types based on latitude |
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altidude (vertical zonation) |
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changes in system type based on altitude are similar to changes based on latitude |
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primary bases of classification of biome |
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vegetation type - forest, grassland shrubland |
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any disruption of a functioning ecosystem |
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types of disturbance to ecosystem |
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volcanic activity hurricane tsunamis drought fire invasive species |
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non-native transplant of species replaces existing species with an ecosystem disrupt existing balance - change in ecosystem dynamic |
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competative exclusion principle |
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no two species can occupy the same niche within a single ecosystem |
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disturbance is total - complete removal of existing biota result of initiating disturbance |
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generally small, highly adaptive plants that prepare way for transition to next stage of recovery |
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succession process builds on surviving biota - both plants and animals |
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gradual expansion of niche and habitat leading to increasingly complex ecosystem |
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various stages of disturbance and recovery |
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local obliteration of habitat - initiating disturbance bare ground, logging roads and skid trails lead to increased erosion disrupt migration and/or foraging pattern of animals |
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removal of forested land for purposes of conversion to new use clear cutting/burning |
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human perception of natural hazards |
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understanding natural hazard risk natural hazard risk communication evacuation vulerability blame and denial preparation, prevention and mitigation |
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normal and natural occurences that are the result of fluctuations in the environment |
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rare and unusual events of large scale proportions and devistation |
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public believes that it is possible to be completely safe and have risk completely removed |
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1% annual exceedance probability flood |
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how close a population is to a hazard and what the physical conditions surrounding that hazard are |
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how well a population is protected against a hazard |
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how well a population can cope and recover after a disaster incident |
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socual vulnerability index |
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what segments of the population will lose the most in a disaster |
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preparing for an emergency by one's own initiative, rather than government order |
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residents can accept that disasters happe to other people in other places but will still deny that it can happen to them |
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what can we do to prepare for natural disaster? |
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Definition
preparation - community drills, evacuation plans, emergency supply packs prevention mitigation |
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taking action to make negative effects or repercussions of hazards less severe -leave hazardous areas underdeveloped or use for alternative purposes -charge land developers a fee that will go towards emergency education or recovery funds |
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3 determinants of aridity |
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Definition
1. zone of subtropical high pressure - descending warm, dry air mass, seasonal variation 2. leeward side of mountain 3. continental interiors |
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mountain glaciers result of cold weather at high elevation |
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