Shorelines.

Slides:



Advertisements
Similar presentations
Features of EROSION & Features of DEPOSITION
Advertisements

Wave Erosion 16.2 Review.
CH 16 The Dynamic Ocean Ocean water is in constant motion and powered by many forces Forces include wind, Coriolis, gravity, density differences Ocean.
Erosion and Deposition Ryan, Jack, Brooke, Jordan, and Becca
The Restless Ocean.
Earth Science 16.3B Shoreline Erosional Features
Chapter 11: The Coast: Beaches and Shoreline Processes
Waves, Beaches, and Coasts Prepared by Betsy Conklin for Dr. Isiorho.
Shoreline Features.
Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125.
Chapter 15 Section 3 By- Robert Sterling, Sam Dixon, Ryan McCarthy, Mikaela Cormier, and Sarah Fournier.
© 2012 Pearson Education, Inc. Earth Science, 13e Tarbuck & Lutgens.
Chapter 10 The Restless Ocean
COASTLINES Aquatic Science
Definitions of Coastal Regions: The shore is the area on the coast which covers the furthest low tide mark to the highest elevation where waves affect.
Shores and coastal processes. Goal To understand how coastal processes shape shores and coastlines and how these processes affect people.
16.3 Shoreline Processes and Features
(The Coastal Zone and Waves)
Glacier Landforms Wave Erosion Shorelines are being constantly eroded by waves, tides, and chemical weathering. Sea cliffs are produced.
Copyright © 2007 Pearson Prentice Hall, Inc. 1 Geology 4th edition by Chernicoff & Whitney Chapter 19 Shores and Coastal Processes Chapter 19 Shores and.
Coastal Zones and Processes
Key Questions for Understanding Section 16.1
© 2011 Pearson Education, Inc. Earth: An Introduction to Physical Geology, 10e Tarbuck & Lutgens.
Unit 1: Land and Water Forms Wearing Down Landforms Wind and Waves
Coastal Deposition. Parts of a beach Coastal Transport The water that hurtles up the beach as a wave breaks is called swash. The water that returns to.
The Dynamic Ocean Chapter 15
Wave Erosion and Deposition
World Geography Unit 1: Land and Water Forms Wearing Down Landforms Wind and Waves.
Characteristics of Waves
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
Sc.912.e.6.4 Analyze how specific geologic processes and features are expressed in Florida and elsewhere.
Coastal Geology: Part I Forces Affecting Shoreline Development Nick Warner.
Friday April 8, 2011 (Shoreline Features; Stabilizing the Shore; Coastal Classification)
Tuesday March 27, 2012 (The Coastal Zone and Waves)
Starter Complete the # 5-8 on page 4 of the sheet entitled, “Standardized Test Prep”. Answer all questions to the best of your ability. You may write on.
Warm Up 1)Which of the following is a tidal current? a. spring tidec. neap tide b. flood tided. both a and c 2)The smallest daily tidal range occurs during.
What forces shape a shoreline?
Coasts. Wave erosion coasts formed by the force of waves as they strike the land the waves strike the land and pieces of rock are broken off the wave.
Wave Erosion.
April 6, 2014.
Shorelines Chapter 20.
Powerpoint Presentation Earth: An Introduction to Physical Geology, 7e
Erosion and Deposition
…and Shoreline Development
Wave action and coastal landforms
Shoreline Features and Processes
Our Beaches Are Funky Strange shapes.
Coastal Depositional Landforms
CH 16 The Dynamic Ocean Ocean water is in constant motion and powered by many forces Forces include wind, Coriolis, gravity, density differences Ocean.
Coastal Processes WHAT am I?
Chapter 10 The Coast: Beaches and Shoreline Processes
Waves and the Shore.
Shoreline Processes and Features
16.3 – Shoreline Processes and Features
The Coast: Beaches and Shoreline Processes
Shorelines.
Wave refraction and waves breaking into surf
Shoreline Features.
Coastal Processes Understanding coastal processes is important when trying to preserve and protect beaches In Florida, 75% of the population (10.5 million)
The Restless Ocean.
Shorelines.
Shorelines.
River Erosion Erosion shapes the land in different ways as the river moves from its source to its mouth: Near the source of a river, in the upper course,
Coastal Geology Erosional Shore Features.
Wave Erosion Chapter 4.3.
Beach Erosion.
Shoreline Processes and Features Outline
Shoreline Processes and Features
Beach Erosion.
Coastal Processes.
Presentation transcript:

Shorelines

The shoreline: A dynamic interface The shoreline is a dynamic interface (common boundary) between air, land, and the ocean The shoreline is constantly being modified by waves Today the coastal zone is experiencing intense human activity

Shoreline features Features vary depending on several factors including The rocks along the shore Currents Wave intensity Whether the coast is stable, sinking, or rising

Shoreline features Features associated with headlands Sea cave Sea arch Sea stack

Refraction of waves

Wave energy concentrated on headlands begins eroding a Sea Cave. When the cave reaches through the headland it forms a Sea Arch.

When the top of the arch falls, if forms a Sea Stack. Not to be confused with a sleestack.

Movement of sand by longshore current

Features related to beach drift and longshore currents Spits Elongated ridges of sand extending from the land into the mouth of an adjacent bay Often the end of a spit hooks landward in response to wave-generated currents forming a hook.

Shoreline features Baymouth bar – a sand bar that completely crosses a bay

Depositional features along the coast of Massachusetts

Shoreline features Barrier islands Mainly along the Atlantic and Gulf coasts Low ridges of sand that parallel the coast 3 to 30 kilometers offshore Probably form in several ways If the shoreline remains stable, the result of shoreline erosion and deposition is to eventually produce a straighter coast

Barrier islands along the Texas coast

Shoreline erosion problems Three basic responses to erosion problems Building structures Jetties Usually built in pairs to develop and maintain harbors Extend into the ocean at the entrances to rivers and harbors

Jetties are built to prevent deposition in navigation channels

Shoreline erosion problems Three basic responses to erosion problems Building structures Groins Built to maintain or widen beaches Constructed at a right angle to the beach to trap sand

Shoreline erosion problems Three basic responses to erosion problems Building structures Breakwater Barrier built offshore and parallel to the coast Protects boats from the force of large breaking waves

Shoreline erosion problems Three basic responses to erosion problems Building structures Seawall Barrier parallel to shore and close to the beach to protect property Stops waves form reaching the beach areas behind the wall Often the building of structures is not an effective means of protection

Emergent and submergent coasts Emergent coasts Develop because of uplift of an area or a drop in sea level Features of an emergent coast Wave-cut platforms

Emergent and submergent coasts Caused by subsidence (sinking) of land adjacent to the sea or a rise in sea level Features of a submergent coast Highly irregular shoreline Drowned valleys

Chesapeake Bay is a good example of a submergent coastline