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Coasts - Key Ideas l are temporary structures, often subject to rapid change. l The location of a depends on tectonic activity and the level of water in the . l Coasts are classified as primary or secondary. l Human interference in coastal processes rarely increases the long term stability of a coast.

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Classifying Coasts

Coasts can be classified by a method that takes into account tectonic position and level.

Primary coasts are young coasts dominated by terrestrial influences.

Secondary coasts are older coasts that have been changed by marine influence.

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Types of Primary Coasts

• Drowned

• Coasts built out by processes (e.g., rivers, glaciers)

• Volcanic coasts

• Coasts shaped by tectonic processes

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Primary Coasts

Many of the of Martha’s Vineyard and are 4 examples of a primary coast.

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Processes Shaping Coasts

• Waves and currents

• Stream

• Wind

• Freeze/thaw cycles

• Slumping

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Secondary Coasts

Waves are one of the that shape secondary coasts. 6

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Alternative Classification of Coasts l Erosional Coasts

l Features are: , cliffs, stacks, arches, wave-cut platform l Depositional Coasts

l Features are: barrier islands, deltas, glacial deposits

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Other Types of Coasts l Drowned Coasts

l , fiords l Emergent or Uplifted Coasts

l Uplifted marine terraces l Coasts affected by organisms

l Reefs,

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Beaches

A is a zone of loose particles that covers a .

Note that larger particles are associated with more sloped beach.

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Features of

• berm • berm crest • backshore • foreshore • beach scarp • longshore trough • longshore bars

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Beaches

The features of a beach.

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Wave Refraction and Longshore

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Longshore Drift l Features formed by

l , , l Human interference with longshore drift

l Jetties, groins, breakwaters l Sources of

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Large Scale Features of Secondary Coasts

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Origin of Barrier Islands

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Coastal Cells

Sections of coast in which sand input and sand output are balanced are referred to as coastal cells. 25

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Coasts Formed by Biological Activity

Coral Reefs are the most dramatic of the coasts formed by biological activity.

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Coral Classifications

Fringing Reefs cling to the margin of land.

Barrier Reefs are separated from land by a .

Atolls are ring-shaped islands of enclosing .

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Storm Surges

A is an abrupt bulge of water driven on shore by a tropical cyclone or a frontal storm.

Storm surges are short-lived.

Storm surges consist of only a crest, so they cannot be assigned a period or wavelength, and cannot be called a wave.

Storm surges are sometimes called storm .

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Human Interference on Coastal Processes

• Groins

• Importing sand

These methods are largely ineffective in solving beach erosion.

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Coasts

A map showing shore erosion by region. One example of shore erosion is the lighthouse on Hatteras, which was moved during 1998 and 1999 to protect it from destruction. It was threatened by rising sea levels and a changing shoreline.34

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Characteristics of U.S. Coasts

The Pacific Coast - An actively rising margin where indications of recent tectonic activity can be observed.

The Atlantic Coast - A on the trailing position of the North American plate.

The Coast - Smaller wave size and a smaller characterize the Gulf Coast.

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Summary

A few of the many types of measures taken to slow and prevent beach erosion. Some of these methods are actually counterproductive.

In many cases these methods help serve as a reminder that shorelines and beaches are constantly changing, and are not under human control.

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Estuaries

An is a in which fresh water mixes with ocean water. Estuaries can be classified by their origin.

• Drowned river mouths

• Bar-built

• Tectonic

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Estuaries

The four types of estuaries. 39

Salt-Wedge Estuary (river-dominated)

Examples: Mouths of Mississippi, Hudson and Columbia Rivers

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Well-Mixed Estuary (-dominated)

Examples: Shallow estuaries such as Chesapeake and Delaware Bays

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Partially Mixed Estuary

Examples: Puget and San Francisco

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Fjord-Type Estuary

Examples: Glaciated coastal mountains

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Estuarine Water Budget

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Positive Water Balance Estuary

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Negative Water Balance Estuary

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