World Geography 3200/3202. Outcomes In this section you will: 1.5.1 Define the term spit. (k) 1.5.2 Define the terms sea cave, sea arch, and stack. (k)

Slides:



Advertisements
Similar presentations
WS 7.1, Page 21 1a) Strength of wind and fetch affect the size of waves. The stronger to wind, the larger the size of waves. The longer the distance over.
Advertisements

Features of EROSION & Features of DEPOSITION
Wave Erosion 16.2 Review.
Coastal Erosion and Management At Reculver In Kent
Slow Changes to Earth’s Surface
Wave action is the primary means of erosion along coastlines.
OCEAN WAVES CHANGE COASTLINES.
COASTAL LANDFORMS.
FEATURES OF SEA EROSION AND DEPOSITION
Section 2: Wave Erosion Preview Key Ideas Shoreline Erosion Beaches
1.5Understand how ocean waves and currents change the face of coastal areas.
Shoreline Features Ch These notes go on p. 19 of your INB!
16.3 Shoreline Processes and Features
World Geo 3200/3202 November Introduction In this lesson you will: Define the terms sea cave, sea arch, and stack. (k) Explain how sea.
1.5Understand how ocean waves and currents change the face of coastal areas. (Chapter 3)
Coastlines. I. Waves A. Wave anatomy I. Waves A.Wave anatomy B. Wave Erosion Corrosion, 2) Abrasion, 3) Hydraulic Action.
Coastal Processes ~ erosion, transport & deposition
An introduction to coasts. What is the difference between weathering and erosion? Weathering is the wearing away of rocks. Erosion is when the loose.
Unit 1: Land and Water Forms Wearing Down Landforms Wind and Waves
Wave Erosion and Deposition
World Geography Unit 1: Land and Water Forms Wearing Down Landforms Wind and Waves.
Characteristics of Waves
WAVE EROSION. How do waves form? By wind that blows across the water’s surface. The wind causes water particles to move up and down as a wave goes by.
Ocean Wave and Current Erosion
Waves and Coasts waves Agents of erosion as get closer to shore: –wavelength decreases –velocity decreases –amplitude increases –in shallow water,
Erosion and Deposition
Coasts.
Sc.912.e.6.4 Analyze how specific geologic processes and features are expressed in Florida and elsewhere.
Coastal Processes. - Creating waves - Constructive waves - Destructive waves - Processes of erosion - Processes of transportation - Longshore drift -
Coastal Features Headlands and Bays A headland is an area of land which juts out to sea and is surrounded by sea on three sides. Headlands form in coastlines.
What do you see in this picture?
What are sub-aerial processes and why are they important? What processes of erosion operate at the coast? What landforms are created by erosion? What.
1.5.4Understand how ocean waves and currents change coastlines. (Chapter 3)
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.
COASTAL EROSIONAL AND DEPOSIONAL FEATURES
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.
Agents of Erosion and Deposition Devils Tower, WY icformations.htm.
MLO 5:Coastal Processes. Wave Erosion Hydraulic pressure = The pounding force of water/waves. Corrosion = Minerals such as calcium carbonate & limestone.
Describe how sea caves are formed. (P. 48)
Erosion and Deposition
Headlands and Bays Coastal Features
Wave action and coastal landforms
Shoreline Features and Processes
By Angelos Petrou & Christos Kathidjiotis
Shorelines.
1. 8. Understand how ocean waves. and currents change the face
Coastal Processes WHAT am I?
Warm-up Week 4 The vertical distance between trough and crest is called the ____. a. wave height c. fetch b. wavelength d. wave period A fetch is _________.
Waves and the Shore.
Shoreline Processes and Features
16.3 – Shoreline Processes and Features
Erosion: solution Sea water is slightly acidic and dissolves soluble material from the rock. Sea water dissolves rocks made of calcium carbonate such as.
Wave refraction and waves breaking into surf
Shoreline Features.
Go through and highlight important information.
Warm-up Week 4 The vertical distance between trough and crest is called the ____. a. wave height c. fetch b. wavelength d. wave period A fetch is _________.
The Restless Ocean.
What’s going on ?.
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,
“Shoreline Processes”
Transportation and deposition
Waves Section 9.5.
Coastal Landforms: Erosional and Depositional
Headlands and Bays Coastal Features
Wave Erosion Chapter 4.3.
Shoreline Processes and Features Outline
Coastal Processes.
Presentation transcript:

World Geography 3200/3202

Outcomes In this section you will: Define the term spit. (k) Define the terms sea cave, sea arch, and stack. (k) Explain how sea caves, sea arches and stacks are formed. (a) Analyze the processes that result in the “straightening out” of an irregular coastline. (a)

Water/Wave Erosion Concepts Three Weathering Terms 1. Hydraulic pressure: The pounding force of water/waves 2. Corrosion: Minerals such as calcium carbonate and limestone dissolve in the water 3. Abrasion: rock and sand particles suspended in the water bump, grind, scrape and gouge surfaces the water hits.

Water/Wave Erosion Concepts Longshore Drift Terms 1. Headlands: the protrusions of land that extend the farthest out into wave action. 2. Longshore drift: refers to the fact that dominant waves have enough energy to carry silt/sand from headlands along the shore where it is later deposited. 3. Wave Refraction: waves bending around headlands as they hit the shallow water by shore

Straightening an Irregular Submerging Coastline Irregular submerging coastlines have headlands that protrude out from the shore line. The erosion of the headland can deposit silt in the bay which forms a bay beach as it tends to reduce the irregularity of the coastline. The headland is reduced due to erosion and the bay is being filled by deposition.

Straightening an Irregular Submerging Coastline Longshore drift results in some sand being deposited parallel to the shore but connected to the headland. These silt deposits are known as spits. Longshore drift and deposition can continue to the point that the spit closes off the mouth of the bay. This extensive deposit is known as a bay bar. As you can see it tremendously reduces the irregularity in the coastline. Continued erosion and deposition can straighten a coastline over a long period of time.

Straightening an Irregular Submerging Coastline Sketch the following diagrams to help with your understanding of the steps for straightening an irregular coastline

Assigned Readings "Wave Movement and Direction" on pages 41-42; "Effects of Wave erosion and Deposition" on pages

Case Study Assigned Readings "CASE STUDY the Curonian Spit" on pages Assigned Activities Complete Question #17 on page 46.