Montessori for Everyone 2013 Types of Coastlines
|
|
- Dustin Bryan
- 6 years ago
- Views:
Transcription
1 Coast The coast is the part of the land that borders the sea. It is subject to constant change, as the result of the waves and deposits carried by water onto the land. Coastline The coastline is where the land and the sea merge. Because the actual line changes with the tides, some scientists refer to this area as a coastal zone. Regular Coastline Regular coastlines have a smooth outline with few to no natural harbors. If there are mountains inland, the regular coast usually runs parallel to them. Irregular Coastline A coast is irregular when the line of the land is uneven, containing many natural harbors. The harbors enable trade, and can help a country thrive. Please note: These are not 3-part cards and are not meant to be. They are information cards. When you cut them apart, cut only on the black lines. Do not cut apart the picture, name, and definition. Please see the instructions at the end for how they are to be used.
2 High Coastline The coast is described as high when the land descends vertically to the sea. It can be regular (smooth) or irregular, with many harbors and bays. Low Coastline The coast is described as low when the land gradually descends to the sea. It can be regular (smooth), or irregular, with many harbors or bays. Emergent Coastline Emergent coastlines are exposed to the sea due to falling sea levels, caused by shifting tectonic plates of the Earth, or a global change in sea level. Submergent Coastline When the sea level rises because of shifting tectonic plates of the Earth or a global change in sea levels, the resulting coast is a submergent coastline.
3 Low Sandy Coastline A coastline whose land descends gradually to the sea, and is made mostly of sand, is called a low sandy coastline. Low Rocky Coastline A low rocky coastline is a made mostly of rocks and rocky matter and descends gradually to the sea. Promontory A promontory is an irregular coastline of emergence. A mountainous point of land that protrudes into the sea, it is usually high with a sheer drop and rocky cliffs. Peninsula A peninsula (or headland) is an irregular coastline of emergence. It is a large stretch of land surrounded by water on almost all sides.
4 Cape A cape is an irregular coastline of emergence, consisting of land surrounded by water. It is larger than a point but not as large as a peninsula. Point A point is an irregular coastline of emergence, consisting of tapering land that projects into the water. It is often formed by the deposit of silt by ocean currents. Spit A low-lying narrow piece of land projecting into the sea, usually at the entrance to a bay, is called a spit. It is an irregular coastline of emergence. Isthmus A piece of land that connects two other pieces of land is called an isthmus. It is an irregular coastline of emergence.
5 Gulf A gulf is part of an irregular coastline of submergence. It is a very large area of water partially surrounded by land. It is larger than a bay. Fiord (Fjord) A fiord (fjord) is an irregular coastline of submergence. It is a long, deep, narrow inlet of the sea often bordered by steep cliffs. It is carved by a glacier. Bay A bay is part of an irregular coastline of submergence. It is an indentation in a sea or lake where water is surrounded by land. It is not as big as a gulf. Cove A cove is a small bay or inlet, consisting of water that indents into the land. It is part of an irregular coastline of submergence, and is often circular or oval.
6 Harbor A harbor is an irregular coastline of submergence. It is a small bay or other sheltered part of a larger body of water, deep enough for ships to anchor. Ria A ria is a kind of irregular coastline of submergence. Rias occur when the sea level rises near a valley, flooding it. A ria is also called a drowned river valley. Strait A strait is an irregular coastline of submergence. It is a narrow stretch of water which connects two larger bodies of water.
7 Types of Coastlines Coast Coastline Low Coastline High Coastline Regular Coastline Irregular Coastline Low Irregular Coastline* Low Regular Coastline* Low Sandy Coastline Low Rocky Coastline High Irregular Coastline* High Regular Coastline* Submergent Coastline: Gulf Fiord/Fjord Bay Cove Harbor Ria Strait Emergent Coastline: Peninsula Promontory Cape Point Spit Isthmus *These types are mentioned in the definitions but are not individually pictured. Montessori for Everyone 2013 Types of Coastlines Control Chart
8 Instructions Instructions for making this item: print on cardstock, laminate, and cut cards apart. There were two reasons why we did not make these cards in the traditional 3-part card style: 1. The cards have a hierarchy some of them represent larger categories while others fall under those categories. It s hard to arrange them correctly by hierarchy when they are 3-part cards. 2. Many of the coastlines look extremely similar, making it difficult to match the name and definition to the picture. When students work with this material, have them read the name and definition on each card and place it on a rug, roughly following the outline on the control chart. This lets them see which coastlines are subtypes of other types. These cards are for 9-12 year olds who have already completed basic Geography work (Land and Water Forms, Advanced Land and Water Forms, Parts of a River, Mountain, and Volcano, as well as studies of countries and continents). The study of Types of Coastlines is part of the horizontal configuration of the Earth, as opposed to the vertical configuration (layers of the Earth, layers of the Earth s surface, layers of the atmosphere). There are other features that occur at coastlines that are not types of coastlines but are related. An interested student might want to study them. Here are a few suggestions: lagoon sea caves jetty stack channel stump salt marsh delta canal estuary dunes shoal beach Our Geographic Features Research Guides (found in the Research Guide section of our store/cd) has a research guide for studying coastlines which would be a nice companion to these cards.
Overview. Beach Features. Coastal Regions. Other Beach Profile Features. CHAPTER 10 The Coast: Beaches and Shoreline Processes.
Overview CHAPTER 10 The Coast: Beaches and Shoreline Processes Coastal regions constantly change. The beach is a dominant coastal feature. Wave activity continually modifies the beach and coastal areas.
More informationCOASTAL SYSTEMS WAVE ENERGY
WAVE ENERGY The energy of a wave determines its ability to erode and transport material on the coast Wave energy depends on the fetch, the distance the wind has blown the wave Wind strength and wind duration
More informationChapter 12: Coasts (after a brief review of Tides)
Chapter 12: Coasts (after a brief review of Tides) 1 Questions from previous classes: What happens when a wave meets a current? wave = people walking current = bus If wave goes with the current, the wave
More information1.5 Understand how ocean waves and currents change the face of coastal areas. (Chapter 3)
1.5 Understand how ocean waves and currents change the face of coastal areas. (Chapter 3) 1. Hydraulic Action/Pressure - air being forced into crack in rocks. 2. Corrosion (Solution) Minerals such as calcium
More informationShore - place where ocean meets land Coast - refers to the larger zone affected by the processes that occur at this boundary.
Waves, Beaches, and Coasts Shore - place where ocean meets land Coast - refers to the larger zone affected by the processes that occur at this boundary. Waves: energy moving through water The height of
More informationEssentials of Oceanography Eleventh Edition
Chapter Chapter 1 10 Clickers Lecture Essentials of Oceanography Eleventh Edition The Coast: Beaches and Shoreline Processes Alan P. Trujillo Harold V. Thurman Chapter Overview Coastal regions have distinct
More informationChapter 10 Lecture Outline. The Restless Oceans
Chapter 10 Lecture Outline The Restless Oceans Focus Question 10.1 How does the Coriolis effect influence ocean currents? The Ocean s Surface Circulation Ocean currents Masses of water that flow from one
More informationChapter - Oceans and Coasts
Chapter - Oceans and Coasts Discussion: What do oceans contribute to the environment of Earth? How do Earth s major systems relate to the oceans? Oceans and Coasts Oceans are important - Thermal regulation
More information1.5 How do ocean waves and currents change the face of coastal areas? (Chapter 3)
1.5 How do ocean waves and currents change the face of coastal areas? (Chapter 3) 1. Hydraulic Action/Pressure - air being forced into crack in rocks. 2. Corrosion (Solution) Minerals such as calcium carbonate
More informationDraw a picture of a water source. Don t forget to include yourself in the picture!
Name Date Draw a picture of a water source. Don t forget to include yourself in the picture! My water source is Students describe the characteristics of a water source: stream, river, lake, pond, ocean,
More informationOceans and Coasts. Chapter 18
Oceans and Coasts Chapter 18 Exploring the oceans The ocean floor Sediments thicken and the age of the seafloor increases from ridge to shore The continental shelf off the northeast United States Constituent
More informationCoastal management has lagged behind the growth in population leading to problems with pollution
Fifty percent of the population of the industrialized world lives within 100 km of a coast. Coastal management has lagged behind the growth in population leading to problems with pollution and natural
More informationLecture Outlines PowerPoint. Chapter 15 Earth Science, 12e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 15 Earth Science, 12e Tarbuck/Lutgens 2009 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
More informationMarginal Marine Environments
Marginal Marine Environments Delta: discrete shoreline protuberances formed where rivers enter oceans, semi-enclosed seas, lakes or lagoons and supply sediment more rapidly than it can be redistributed
More informationpage - Laboratory Exercise #5 Shoreline Processes
page - Laboratory Exercise #5 Shoreline Processes Section A Shoreline Processes: Overview of Waves The ocean s surface is influenced by three types of motion (waves, tides and surface currents). Shorelines
More informationCoastal Change and Conflict
Coastal Change and Conflict Outline of the Topic Contrasting Coasts why do all coasts not look the same? Geology of the coast the impact rock structure has on the coastline Waves Constructive and destructive
More informationGeneral Coastal Notes + Landforms! 1
General Coastal Notes + Landforms! 1 Types of Coastlines: Type Description Primary Coast which is essentially in the same condition when sea level stabilized Coastline after the last ice age, younger.
More informationNearshore Sediment Transport What influences the loss of sediment on Beaches? - Waves - Winds - Tidal Currents - River discharge - Runoff
Tides & Beaches Nearshore Sediment Transport What influences the loss of sediment on Beaches? - Waves - Winds - Tidal Currents - River discharge - Runoff Oceans Ocean Topography Physical Structure of the
More informationThere are many different kinds of beaches which are generally characterized by the dominance of waves, tides, rivers and currents, and in particular
Fig. 11-11, p. 253 There are many different kinds of beaches which are generally characterized by the dominance of waves, tides, rivers and currents, and in particular differ by the amount of energy, which
More informationThe Case of the Disappearing Shoreline
Name The Case of the Disappearing Shoreline Humans change the earth's climate in many ways. One change is the increase of carbon dioxide in the atmosphere. As we burn more fossil fuels, we release more
More informationCoasts. 1. Coastal Processes. 1.1 Coastal erosion. 1.2 Sediment transport. Coastal Processes and Landforms. i. Hydraulic action
Coasts Coastal Processes and Landforms 1. Coastal Processes 1.1 Coastal erosion i. Hydraulic action When waves strike against a rock surface, the waves trap air in the rock joints. This air is compressed
More informationShorelines Earth - Chapter 20 Stan Hatfield Southwestern Illinois College
Shorelines Earth - Chapter 20 Stan Hatfield Southwestern Illinois College The Shoreline A Dynamic Interface The shoreline is a dynamic interface (common boundary) among air, land, and the ocean. The shoreline
More informationReading Material. Inshore oceanography, Anikouchine and Sternberg The World Ocean, Prentice-Hall
Reading Material Inshore oceanography, Anikouchine and Sternberg The World Ocean, Prentice-Hall BEACH PROCESSES AND COASTAL ENVIRONMENTS COASTAL FEATURES Cross section Map view Terminology for Coastal
More informationChapter 20 Lecture. Earth: An Introduction to Physical Geology. Eleventh Edition. Shorelines. Tarbuck and Lutgens Pearson Education, Inc.
Chapter 20 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Shorelines Tarbuck and Lutgens The Shoreline: A Dynamic Interface The Coastal Zone The shoreline is constantly modified by
More informationMAPS AND AERIAL PHOTOS REVISION
MAPS AND AERIAL PHOTOS REVISION IF THE FOLLOWING COMES UP IN THE SHORT QUESTIONS REMEMBER SCALE OF 1:1,100,000,000 MAP FROM A WORLD ATLAS LARGE AREAS WITH LITTLE DETAIL 1:250,000 SCALE OF CAR ATLAS MAP
More informationTITLE: COASTAL EROSION AND LANDFORMS.
TITLE: COASTAL EROSION AND LANDFORMS. AIM: What are the factors that influence the formation of coastal features along Fishing Pond beach Trinidad? LOCATION OF FIELD STUDY: The study was carried out in
More informationTypes of Estuaries and Mixing Patterns. Mrs. Stahl Marine Science Honors
Types of Estuaries and Mixing Patterns Mrs. Stahl Marine Science Honors Coastal Plain Form between glacial periods, when water from melting glaciers raises the sea level and floods coastal plains and low
More informationLäna i is a single shield that formed from summit eruptions and along
Läna i is a single shield that formed from summit eruptions and along three rift zones between 1.2 and 1.46 Ma; a classic example of a Hawaiian shield with a gently sloping profile. The small sub-circular
More informationEstuaries: Life on the Interface
Material adapted from: Estuaries: Interface between sea and land & Sea Margin Diversity, The Water Sourcebook Grades 9-12, EPA http://www.epa.gov/safewater/kids/wsb/ Introduction: Some of the most dynamic
More informationCOASTAL ENVIRONMENTS. 454 lecture 12
COASTAL ENVIRONMENTS Repeated movement of sediment & water constructs a beach profile reflecting the balance between average daily or seasonal wave forces and resistance of landmass to wave action Coasts
More informationShorelines Earth Chapter 20 Chapter 20 Shorelines The Shoreline: A Dynamic Interface Cape Cod and Point Reyes Hurricane Sandy
1 2 3 4 5 6 7 8 9 10 11 12 13 Shorelines Earth Chapter 20 Chapter 20 Shorelines The Shoreline: A Dynamic Interface The interface is the common boundary where different parts of a system interact. The Coastal
More information/50. Physical Geology Shorelines
Physical Geology Shorelines Multiple Guess: (You know the drill 2 points each) 1. The path of movement of a water particle in a wave at sea is 1. circular 2. horizontal 3. vertical 4. elliptical 5. none
More informationTidally influenced environments. By Alex Tkaczyk, Henrique Menezes, and Isaac Foli
Tidally influenced environments By Alex Tkaczyk, Henrique Menezes, and Isaac Foli Goals and aims Describe the role of tidal influence in depositional environments. - Deltas - Estuaries Provide an overview
More informationUnder the Boardwalk: Coastal Geomorphology
Under the Boardwalk: Coastal Geomorphology What to look for while you're on the beach during spring break. What Causes Changes in Sea Level? Answer Varies with Time Scale. Long-Term Changes in Sea Level
More informationThe Sea Geography Notes JC-Learn. JC-Learn. Geography Notes The Sea. 1 P a g e
JC-Learn Geography Notes The Sea 1 P a g e The Sea *Here, you can choose to study the chapter on glaciation or the one on the sea, or even both, because whenever these topics come up in the Junior Cert
More informationDefine the key terms: - Abrasion - Attrition - Hydraulic action - Solution. Y11 Coasts
Define the key terms: - Abrasion - Attrition - Hydraulic action - Solution Abrasion caused by waves picking up material which is forced against the cliff face wearing it away Attrition where stones and
More informationMonterey Peninsula College
Introduction to Google Earth Name Goals 1. To become proficient at using the basic features of Google Earth. 2. To recognize differences in coastal features between the east and west coast of North America.
More informationStudland Bay Context and Learning Aims
Studland Bay Enquiry 7: How are coastal processes affecting Studland Bay? Context and Learning Aims Pupils will be supported in and outside of the classroom to: Identify; describe and explain the physical
More informationAnatomy of Coastal Regions
The Coast I. BEACH ANATOMY Anatomy of Coastal Regions Terms for different parts of beaches and coastal regions Are all about ENERGY- ie, where the ocean s energy Mostly through tides and waves, and shape
More information4/20/17. #30 - Coastlines - General Principles Coastlines - Overview
Writing Assignment Due one week from today by 11:59 pm See main class web pages for detailed instructions Essays will be submitted in Illinois Compass (instructions later) Pick one: Earthquakes, tsunamis,
More informationThe Composition of Seawater
The Composition of Seawater Salinity Salinity is the total amount of solid material dissolved in water. Most of the salt in seawater is sodium chloride, common table salt. Element Percent Element Percent
More informationCoastal issues: Beaches and Estuaries. Recent Sea Level: Beaches: Baltimore D.C. Patomac R. Chesapeake Bay
Coastal issues: Beaches and Estuaries Definitions: Coast = broad zone where both marine & terrestrial processes act It includes the beach, lagoons, marshes, bars etc. Coastal processes act to shape the
More informationBEACH PROCESSES AND COASTAL ENVIRONMENTS
BEACH PROCESSES AND COASTAL ENVIRONMENTS COASTAL FEATURES Cross section Map view TOPICS: Terminology Waves Beach Morphology Barriers Coastal Migration Tides Tidal Flats and Marshes Sediment Budgets Human
More informationThe Movement of Ocean Water. Currents
The Movement of Ocean Water Currents Ocean Current movement of ocean water that follows a regular pattern influenced by: weather Earth s rotation position of continents Surface current horizontal movement
More informationGEOLOGY 101 Under the Boardwalk: Coastal Geomorphology
GEOLOGY 101 Under the Boardwalk: Coastal Geomorphology What to look for while you're on the beach during spring break. J.S. Kite, WVU What Causes Changes in Sea Level? Answer Varies with Time Scale. Long-Term
More informationCoastal Processes and Landforms
Coastal Processes and Landforms These icons indicate that teacher s notes or useful web addresses are available in the Notes Page. This icon indicates that the slide contains activities created in Flash.
More informationNYS Coastal Waters. Water Resources of NYS: THE NATURE of the COASTAL ZONE. NYS Coastal Waters. NYS Coastal Atlas. Coastal Zone Management 10/10/2014
Water Resources of NYS: THE NATURE of the COASTAL ZONE NYS Coastal Waters NYS is the only state to border the Atlantic Ocean and the Great Lakes (Lakes Erie and Ontario). Great Lakes shoreline: 577 miles
More informationWHAT ARE ECOSYSTEMS? Dr. V. N. Nayak Professor of Marine Biology (Retd)
WHAT ARE ECOSYSTEMS? Dr. V. N. Nayak Professor of Marine Biology (Retd) An ECOSYSTEM is an interacting system of plant, animals, and humans and the surrounding environment. An ecosystem contains living
More informationImagine that you can see a side view of a wave as it approaches a beach. Describe how the wave changes as the wave approaches the beach.
Geology 101 Name Reading Guide for Ch. 19: Shores and Coastal Processes (p. 612) Waves, Currents, and Tides (p. 614) Waves and Currents (p. 614) Imagine that you can see a side view of a wave as it approaches
More informationCOASTS (P.38-45) Management: Hard engineering: Groynes Sea walls Gabions Soft Engineering: Beach replenishment Dune regeneration
COASTS (P.38-45) Processes: Types of wave Weathering Mass Movement Erosion Transport Deposition Landforms: Cracks Caves Arches Stacks/stumps Headlands/bays Coves Spits Tombolos Beaches Sand dunes Management:
More informationLabel the diagram below with long fetch and short fetch:
Coastal Processes Coasts are shaped by the sea and the action of waves. The processes that take place are erosion, transportation and deposition. The power of waves is one of the most significant forces
More informationFigure 1. Schematic illustration of the major environments on Mustang Island.
STOP #1: PACKERY CHANNEL BEACH TO BAY We will start this field guide near the north jetty of Packery Channel and hike across the island to Corpus Christi Bay (fig. 1). The island emerges from the Gulf
More informationDirected Reading. Section: Ocean Currents. a(n). FACTORS THAT AFFECT SURFACE CURRENTS
Skills Worksheet Directed Reading Section: Ocean Currents 1. A horizontal movement of water in a well-defined pattern is called a(n). 2. What are two ways that oceanographers identify ocean currents? 3.
More informationBeaches Unit (4.5 pts)
T. James Noyes, El Camino College Beaches Unit (Topic 6A) page 1 Name: Section: Beaches Unit (4.5 pts) Beaches and Shorelines Are Always Changing Waves are slowly and inexorably altering the shoreline,
More informationTidal energy is produced by the surge of ocean waters during the rise and fall of tides. Tidal energy is a renewable source of energy.
Encyclopedic Entry For Educator tidal energy For the complete encyclopedic entry with media resources, visit: http://www.connectenergyed.org/education/encyclopedia/tidal-energy/ Tidal energy is produced
More informationLAB: WHERE S THE BEACH
Name: LAB: WHERE S THE BEACH Introduction When you build a sandcastle on the beach, you don't expect it to last forever. You spread out your towel to sunbathe, but you know you can't stay in the same spot
More informationQuestions # 4 7 refer to Figure # 2 (page 321, Fig )
Shoreline Community College OCEANOGRAPHY 101 Fall 2006 Sample Exam # 3 Instructor: Linda Khandro Questions # 1 3 refer to Figure # 1 (page 284, Fig 11.7) 1. At which position is the moon in its new moon
More informationExamples of estuaries include bays, sounds, salt marshes, mangrove forests, mud flats, swamps, inlets, and sloughs.
An estuary is a partially enclosed body of water where incoming seawater is mixed with fresh water coming from the land. Examples of estuaries include bays, sounds, salt marshes, mangrove forests, mud
More informationCh 9: Waves. Wind waves. Formation of a wind wave
Ch 9: Waves 1. Features of Waves 2. Deep-water, shallow water and transitional waves 3. Breaking Waves 4. Wind Waves 5. Tsunamis Cf. Fig. 9-2 Waves are created by a disturbance. * wind (wind waves, L=
More informationChapter 22, Section 1 - Ocean Currents. Section Objectives
Chapter 22, Section 1 - Ocean Currents Section Objectives Intro Surface Currents Factors Affecting Ocean Currents Global Wind Belts (you should draw and label a diagram of the global wind belts) The Coriolis
More informationChesil Beach, Dorset UK High energy, shingle coastline. Brighton Beach, Sussex UK Pebble beach
Beaches: Depositional landform Extends from the highest high tide to the lowest low tide. Very important temporary store in coastal system. Accretion: sediment returning to the visible portion of a beach
More informationSite The fieldwork should be completed at a localised site on the Victorian coast (or elsewhere).
Coastal fieldwork Studying the coast provides the opportunity to conduct fieldwork in coastal regions. This fieldwork could investigate the geographic characteristics of the coast and how they change over
More informationChapter. The Dynamic Ocean
Chapter The Dynamic Ocean An ocean current is the mass of ocean water that flows from one place to another. 16.1 The Composition of Seawater Surface Circulation Surface Currents Surface currents are movements
More informationGCSE GEOGARPHY OCR B REVISION GUIDE Coasts
GCSE GEOGARPHY OCR B REVISION GUIDE Coasts Definition: The interface between land and sea. Coastal regions cover only 10% of the inhabited land space, yet they are home to more than 60% of the world s
More informationEstuarine Shoreline Stabilization
Estuarine Shoreline Stabilization Property Owner s Guide to Determining the Most Appropriate Stabilization Method Estuarine shorelines are dynamic features that experience continued erosion. Land is lost
More information1.1 Coastal processes produce landforms
1.1 Coastal processes produce landforms Types of wave: destructive and constructive Destructive Carry out erosion Tall Powerful High frequency Backwash greater than the swash Take sediment from beach to
More information3/9/2013. Build house on cliff for a view of the ocean - be one with said view Pearson Education, Inc. Shorelines: summary in haiku form
Introduction to Environmental Geology, 5e Edward A. Keller Shorelines: summary in haiku form Chapter 11 Coastal Processes Lecture Presentation prepared by X. Mara Chen, Salisbury University Build house
More informationEarth Science Chapter 16 Section 3 Review
Name: Class: Date: Earth Science Chapter 16 Section 3 Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. The movement of water that parallels the shore
More informationWarm-up # 7 A day 5/17 - B day 5/18 UPDATE YOUR TABLE OF CONTENTS
Warm-up # 7 A day 5/17 - B day 5/18 UPDATE YOUR TABLE OF CONTENTS Question: List all examples of surface water on Earth. Answer: Rivers and streams, lakes and reservoirs, (ponds) wetlands, estuaries and
More informationSUBJECT: EARTH SCIENCE PAPER: THE DYNAMIC EARTH. Code : 27 COASTAL PROCESSES AND LANDFORMS PROF. A. BALASUBRAMANIAN
SUBJECT: EARTH SCIENCE PAPER: THE DYNAMIC EARTH Code : 27 TOPIC: COASTAL PROCESSES AND LANDFORMS BY PROF. A. BALASUBRAMANIAN Objectives After attending this module, the user would be able to understand
More informationEnvironmental Geology Chapter 11 COASTAL PROCESSES and RELATED HAZARDS
Environmental Geology Chapter 11 COASTAL PROCESSES and RELATED HAZARDS Introduction >50% of world population concentrated in the coastal zones ~75% of U.S. population living in coastal states Coastal hazard
More informationCoastal Zones. Coastal Zones
Page 1 of 15 EENS 3050 Tulane University Natural Disasters Prof. Stephen A. Nelson Coastal Zones Coastal Zones A coastal zone is the interface between the land and water. These zones are important because
More informationIdentify one factor which influences wave strength (1 Mark) Factors which affect wave strength
Coasts revision Identify one factor which influences wave strength (1 Mark) Factors which affect wave strength Identify one factor which influences wave strength (1 Mark) Factors which affect wave strength
More informationSection 1: Waves. There are two distinct types of wave at the coastline: constructive and destructive waves.
Coastal Erosion EARTH SCIENCE GEOLOGY COASTAL EROSION Section 1: Waves How do waves form? Waves are generated by the competing forces of surface friction. The wind transfers energy from air to water and
More informationMarine Environments. Copyright 2011 LessonSnips
Marine Environments I must go down to the seas again, for the call of the running tide Is a wild call and a clear call that may not be denied Excerpt from a poem by John Masefield Continents and islands
More informationSTUDY GUIDE. The Land. Physical Geography of Europe. Chapter 11, Section 1. Terms to Know DRAWING FROM EXPERIENCE ORGANIZING YOUR THOUGHTS
For use with textbook pages 271 276. The Land Terms to Know dikes Large banks of earth and stone that hold back water (page 272) polder Drained area of land (page 272) glaciation The process in which glaciers
More informationWaves- how are they formed and how do they affect the coast?
Question 7 Coasts Waves- how are they formed and how do they affect the coast? Waves are caused by friction between the wind and water causing the water to swell. The size and energy of a wave is influenced
More informationMarine Ecosystems. Aquatic Ecosystems Section 2
Marine Ecosystems Marine ecosystems are located mainly in coastal areas and in the open ocean. Organisms that live in coastal areas adapt to changes in water level and salinity. Organisms that live in
More informationUNDERSTANDING YOUR ESTUARY Level IA- ESTUARY SEARCH
UNDERSTANDING YOUR ESTUARY Level IA- ESTUARY SEARCH Kakagon/Bad River Sloughs, a Lake Superior estuary located on the Bad River Reservation near Ashland, WI. GOAL Select one Wisconsin estuary to study
More informationCoastal Processes and Landforms
Coastal Processes and Landforms These icons indicate that teacher s notes or useful web addresses are available in the Notes Page. This icon indicates that the slide contains activities created in Flash.
More informationGEOGRAPHY - STD 8 [ ] Q1.
GEOGRAPHY - STD 8 Movements of Oceans [2016-2017] Q1. Name the two types of regular movements in the oceans. Ans. The regular movements in the ocean are of two types: 1. Horizontal Ocean currents 2. Vertical
More informationCoastal Geomorphology
Orogeny, Epeirogeny,, Climate-Glaciers, Isostasy & Eustacy Favor Glacial Systems, Colluvial Systems, & Clastic Sediments Ice-Age Systems = So Dynamic that Equilibria May Never Be Reached Seaside, Oregon
More informationCoastal Processes Day Criccieth
Coastal Processes Rivers (Conwy) Rivers (Peris) Urban Studies Lowland Glaciation Tourism and National Parks Soils Sand Dunes Upland Glaciation Rural Settlements The Centre and Staff Fieldwork Equipment
More informationConstructive waves build beaches. Each wave is low. As the wave breaks it carries material up the beach in its. material will then be deposited as
Constructive waves Constructive waves build beaches. Each wave is low. As the wave breaks it carries material up the beach in its swash. The beach material will then be deposited as the backwash soaks
More informationLong Beach Island Holgate Spit Little Egg Inlet Historical Evolution Introduction Longshore Transport Map, Survey and Photo Historic Sequence
Appendix B Long Beach Island Holgate Spit Little Egg Inlet Historical Evolution Introduction The undeveloped southern end of Long Beach Island (LBI) is referred to as the Holgate spit as it adjoins the
More informationFOR PERSONAL USE. Shoreline Erosion BROWARD COUNTY ELEMENTARY SCIENCE BENCHMARK PLAN ACTIVITY ASSESSMENT OPPORTUNITIES. Grade 4 Quarter 1 Activity 9
activity 9 Shoreline Erosion BROWARD COUNTY ELEMENTARY SCIENCE BENCHMARK PLAN Grade 4 Quarter 1 Activity 9 SC.D.1.2.4 The student knows that the surface of the Earth is in a continuous state of change
More informationEilat 's artificial lagoons project on the Red Sea - Israel R. Raviv Ir. R. Raviv, Coastal Engineering Ltd., P.O. Box 7322, z/b 37072,
Eilat 's artificial lagoons project on the Red Sea - Israel R. Raviv Ir. R. Raviv, Coastal Engineering Ltd., P.O. Box 7322, z/b 37072, Introduction Eilat city is located in the southern part of the state
More informationControlling Coastal erosion
Controlling Coastal erosion Coastal Erosion Rates in the U.S. Coastal Erosion and Stabilization Economic pressures demanding the stabilization of beaches and coastlines are immense Coastal Erosion and
More informationThe Physical and Human Causes of Erosion. The Holderness Coast
The Physical and Human Causes of Erosion The Holderness Coast By The British Geographer Situation The Holderness coast is located on the east coast of England and is part of the East Riding of Yorkshire;
More informationYour web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore
Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore TIDAL ENERGY For the complete encyclopedic entry with media resources,
More informationWhat is an Estuary? Importance of Estuaries. Importance of Estuaries. Importance of Estuaries
Oceanography 101, Richard Strickland Lecture 20 What is an Estuary? Portion of the ocean that is semi-enclosed by land and diluted by freshwater runoff All estuaries are embayments But embayments without
More informationCHAPTER 8 ASSESSMENT OF COASTAL VULNERABILITY INDEX
124 CHAPTER 8 ASSESSMENT OF COASTAL VULNERABILITY INDEX 8.1 INTRODUCTION In order to assess the vulnerability of the shoreline considered under this study against the changing environmental conditions,
More informationBeach Profiles: Monitoring Sea Level Rise. Student Activity Sheet. Name Date Class
Beach Profiles: Monitoring Sea Level Rise Student Activity Sheet Name Date Class A shoreline is the area where the water and land meet. This is where we find beach: areas where sediments (sand or other
More informationFormation and characteristics of different types of beaches
Activity Title: Formation and characteristics of different types of beaches Focusing questions What different types of beaches are there in New Zealand? How are estuaries different to open coastal sandy
More informationOur Council s Own: Oceanography Cadette/Senior/Ambassador Badge
Our Council s Own: Oceanography Cadette/Senior/Ambassador Badge Oceanography: The science that deals with oceans, the delimitation of their extent and depth, the physics and chemistry of their water, marine
More informationOcean Motion Notes. Chapter 13 & 14
Ocean Motion Notes Chapter 13 & 14 What is a Wave? Wave: movement of energy through a body of water How are Waves Caused? Caused mostly by wind Wind blowing on the water transmits energy to the water Size
More informationWIND SPEED LENGTH OF TIME WIND BLOWS (Duration) DISTANCE OVER WHICH IT BLOWS (Fetch)
WAVES Up and down movement of ocean surface Transportation of energy across the water over vast distances If not stopped by anything, waves can travel entire oceans Size and speed depend upon: WIND SPEED
More informationBeach profile surveys and morphological change, Otago Harbour entrance to Karitane May 2014 to June 2015
Beach profile surveys and morphological change, Otago Harbour entrance to Karitane May 2014 to June 2015 Prepared for Port Otago Ltd Martin Single September 2015 Shore Processes and Management Ltd Contact
More information15 Coasts and Changing Sea Levels
CHAPTER 15 Coasts and Changing Sea Levels PEOPLE LIVE ALONG COASTS for a variety of good reasons. Oceans moderate climate, supply fish and other sea resources, provide transportation for people and goods,
More informationImpacts of breakwaters and training walls
Across the eastern seaboard of Australia, breakwaters and training walls have instigated fundamental perturbations to coastal and estuary processes. This has induced long-term changes to foreshore alignments,
More information