NORTH HAVEN NORTH HAVEN SLSC

Size: px
Start display at page:

Download "NORTH HAVEN NORTH HAVEN SLSC"

Transcription

1 NORTH HAVEN NORTH HAVEN SLSC Patrols: November to March, weekends and public holidays North Haven beach is the product of a major redevelopment of the northern part of the Adelaide coast. In the 1980s, North Haven Marina development excavated a large marina behind the beach, with two breakwaters to protect the entrance. The North Haven beach is now located between the northern breakwater and the older breakwater for Adelaide s Outer Harbour. The 1.2 km long beach is wedged between the two breakwaters and has been slowly building seaward. Residential development backs the beach, with the North Haven Surf Life Saving Club, a large car park and dunes occupying the beachfront. The beach faces southwest and is composed of fine sand, which, together with the low waves, usually less than 0.5 m has produced a wide, flat, firm beach and a wide, shallow bar attached to the beach. Swimming: This is the safest beach on the Adelaide coast, with usually low wave to calm conditions and no rip currents. Surfing: None, except during a huge ocean swell which can penetrate up the gulf as far as North Haven, where it arrives as a low, 0.5 m swell. Fishing: The boundary breakwaters offer the best locations. Summary: A relatively newly developed beach, with good access and parking, plus the surf club, in a low energy setting. SEMAPHORE, LARGS BAY SEMAPHORE SLSC Patrols: November to March, weekends and public holidays At Point Malcolm the Adelaide coast protrudes more than 1 km seaward. The older suburb of Semaphore is located on the point, which, together with Largs Bay, make up 7 km of continuous residential development. This entire area is situated on the Lefevre Peninsula, a 10 km long and up to 1 km wide accumulation of sand, that has been deposited over the past 6000 years by the northern movement of sand from as far south as Seacliff. This movement is continuing today, the results of which are clearly evident in the wide, low dune fronting the beach, the wide beach and multiple shallow bars. The sand is now accumulating under the jetties and against the North Haven breakwater, where the beach has built out 400 m seaward in the past 20 years. The northern Adelaide coast, showing the continuous strip of sandy beaches and shore parallel bars between Tennyson and North Haven. See inserts for details of Semaphore and North Haven. This section of coast receives only low waves, usually less than 0.5 m. Occasional higher waves are sufficient to rework the fine sand into a wide, low, firm

2 beach, fronted by two to three shore parallel shallow bars and troughs, extending up to 500 m seaward of the beach. Swimming: This is a relatively safe section of beach owing to the usually low waves and shallow water. Care need be taken with young children, as the water depth varies over the bars and troughs and there are some deeper holes. Surfing: There is usually no surf up here. You need a very strong south westerly or huge ocean swell to push rideable waves up into Largs Bay. Fishing: The jetties are the most popular spots for fishing, as the beaches are very shallow. Summary: A low energy but still dynamic section of beach that is continuing to grow seaward. There is excellent access and large areas of protected dune, plus the beach and bars to play on. HENLEY SLSC GRANGE SLSC Patrols: November to March, weekends and public holidays North of the Torrens River, the coast runs north northwest for 10 km to the protruding sandy Semaphore foreland, then slowly curves into west facing Largs Bay. This entire 16 km of beach is backed by Adelaide s beach suburbs. It is bounded by the Torrens and North Haven breakwaters, with four jetties crossing the beach. Waves average less than 1 m at the southern Henley Beach and decrease even further north of Semaphore. At the same time, the beach has a continuous attached bar, fronted by a trough then a second bar. Past Semaphore and into Largs Bay a third bar is present, however waves only break on the outer bars during higher wind wave conditions. Under normal low wave conditions, these are all relatively safe beaches. Just be aware of the troughs between the bars if swimming out past the inner bar. Henley Beach is an older suburb with a jetty backed by a plaza and the main shopping area. The Henley Surf Life Saving Club is located 100 m south of the jetty. The entire beach is backed by residential development, including a seawall and road paralleling the back of the beach, with a continuous low tide bar attached to the beach. Grange is another older seafront suburb, with a jetty flanked by old terrace houses and a large car park. The Grange Surf Life Saving Club is located just north of the jetty, adjacent to the terrace houses Swimming: This section of coast is relatively safe inshore and on the attached portions of the inner bar. Care must be taken in the trough, particularly if occupied by currents and on the outer bar. Children sometimes get caught on the bars by the rising tide. Surfing: The surf here depends on the winds, with strong westerlies required to produce a sloppy beach break. Occasionally high outside ocean swell reaches the beaches as a low swell. Fishing: Many fishers use the Patawalonga and Torrens boat ramps to launch their boats for outside fishing, while the two jetties and the Patawalonga Creek mouth are the most popular shore locations.

3 Along the beaches the migrating bars and higher waves produce a range of holes and gutters, which change over time. Summary: A long section of beach with the older Henley and Grange in the centre and newer developments to the north and south. WEST BEACH SLSC Patrols: November to March, weekends and public holidays. West Beach (south) extends from the northern Patawalonga training wall for 1.8 km to the marina breakwater. This beach has been modified in the south by both the training wall, which extends 100 m seaward blocking southerly waves, and the periodic dumping of sand from the build up on the south side of the river. Residential development backs the first kilometre, followed by a sewage treatment works, then a caravan park and marina. The West Beach marina consists of a southern breakwater that provides shelter for the boat ramp. Between the boat ramp and the smaller northern rock groyne is a 50 m long protected sand beach. While this beach is usually calm, it is used for launching boats and jet skis and is often unsuitable and unsafe for swimming because of the boat traffic. The main West Beach faces west and extends for another 2.5 km from the northern marina groyne to the usually closed mouth of the Torrens River. The West Beach Surf Life Saving Club is located at the southern end of the northern residential area, adjacent to the caravan park. Just inside the Torrens breakwater is a large boat ramp which is very popular on weekends. Swimming: The main beach at the surf club offers the best swimming conditions, well clear of the breakwaters, groynes and boat traffic to the south. There are occasional water pollution problems on southern West Beach and at the Torrens River mouth. Surfing: Only during strong onshore winds. Fishing: The training wall, marina breakwater and groyne are all very popular fishing spots. Summary: A beach that has been modified by the river entrance walls and new marina, but still offers 2.5 km of natural beach and the added protection of the patrolled area. GLENELG SLSC Patrols: late October to early April, weekends and public holidays Lifeguard on duty: December to March (Glenelg Brighton) Glenelg is Adelaide s main recreational beach. It is at the end of the tramline and has traditionally been Adelaide s favourite and most accessible beach. It is backed by parks and major hotels and various

4 recreational facilities, including a marina in the river mouth. The Glenelg Surf Life Saving Club is located in the foreshore park, 200 m north of the jetty. The beach terminates at the Patawalonga breakwater, where the breakwater and an artificial reef off the beach have trapped the sand, causing the beach to build over 100 m seaward. Swimming: The Seacliff to Glenelg beaches provide relatively safe swimming, owing to the usually low waves and continuous shallow bar. However rips occasionally cross the bar, scouring deeper channels. Stay on the inner bar and clear of any deeper troughs. Care must also be taken near the rocks at Seacliff, around the two jetties, at currents, and at occasional breaks in the bar where there are deeper holes. The safest swimming is at the four areas patrolled by the Seacliff, Brighton, Somerton and Glenelg Surf Life Saving Clubs. Surfing: Surf is usually low and sloppy along the Adelaide beaches. A high swell in the south or a strong westerly is required to produce waves over 1 m. Fishing: The jetties attract most Brighton and Glenelg fishers, while Seacliff rock flats are also popular, as is the Glenelg breakwater. The water off the beaches tends to be shallow, with the best fishing at high tide. Summary: This is Adelaide s and South Australia s most popular stretch of beach. It offers good access, a wide range of facilities and relatively safe swimming, with usually little surf. SOMERTON SLSC Patrols: late October to early April, weekends and public holidays Somerton Beach is located north of Brighton Beach, beginning at the Minda dunes and extending for 2 km to the north. The Somerton Surf Life Saving Club is located at the northern end of the Minda dunes. At the surf lifesaving club there is a ramp to the beach, with a rock seawall and beachfront road beginning at the ramp and extending all the way to Glenelg. The beach is typically fronted by a continuous attached bar. BRIGHTON SLSC Patrols: late October to early April, weekends and public holidays Brighton Beach extends 1 km either side of the Brighton jetty. The suburb of Brighton is centred on the 200 m long jetty, which is backed by the main street, while the beach to either side is backed by a seawall and road. The Brighton Surf Life Saving Club is located 200 m south of the jetty on the west side of the road. A ramp provides access down the seawall to the beach. SEACLIFF SLSC

5 Patrols: late October to early April, weekends and public holidays Seacliff Beach begins amongst the broad rock flats of Marino Rocks. Several hundred metres north of the rocks, the rock flats thin as the sandy beach increases in extent. By Seacliff Surf Life Saving Club and the adjoining Seacliff Sailing Club, the beach has almost replaced the rocks and a sandy beach continues to Glenelg. In the south the beach is backed by a park below the old Seacliff, then a caravan park and the two club houses, with a car park and boat ramp north of the sailing club. A road and housing then back the beach all the way to Brighton. The beach itself consists of a high tide sand beach and fronting rock flats south of the surf club, with a shallow sand bar replacing the rocks to the north. Waves are low in the south, increasing to about 0.5 m past the clubs. The bar is usually continuous and rips are present only during bigger seas. HALLETT COVE Unpatrolled Hallett Cove is a 1 km long break in the 40 to 60 m high cliffs that dominate the coast from Point Curlew to Seacliff. The break forms a natural amphitheatre along the shoreline, within which is a strip of sand called Hallett Cove Beach The sloping land behind the beach has been partly developed for housing, with a park in the centre of the beach reserve for recreation, the Hallett Cove Surf Life Saving Club and a boat ramp. Field River drains across the southern end of the beach. The beach is 1 km long, faces west and is bordered by the cliffs of Curlew Point to the south and Black Cliff to the north. Black Cliff is a famous geological site where ancient glacial remains are clearly visible. It is now part of the Hallett Cove Conservation Park, which includes the northern half of the beach and bordering cliffs. The cliffs at either end are fronted by 50 to 100 m wide intertidal rock flats. These also extend along the length of the beach, where they are only partially covered by sand at high tide. Consequently the beach, while sandy at high tide, is predominantly rock flats and boulders at low tide, with a sand bar seaward of the rocks. The waves, which average 0.5 to 1 m, break over the bar and rock flats, usually maintaining two to three rips across the bar. Swimming: One has to choose the time and place to swim at Hallett Cove. The best time is high tide when most of the rocks are covered by water and the best place is where most sand is available. The northern end of the beach near Black Cliff has less rocky beds and good sand coverage year round and is preferred by most beachgoers. Surfing: This is not a popular spot owing to the dominance of rocks. Fishing: Most fishing is done from the rocks at either end. The boat ramp is really only useable at high tide, owing to the rocks.

6 Summary: An attractive cove, which unfortunately has lost much of its cover of sand, causing problems for swimmers and surfers. CHRISTIES BEACH SLSC Patrols: November to March, weekends and public holidays Christies Beach occupies the southern third of a 2 km long, west facing beach that extends from Witton Bluff in the south to Curlew Point in the north. The southern half is backed by the growing residential area called Christies Beach, while the northern half is known as O Sullivan Beach and is backed by a sewage treatment works. There is excellent access at Christies Beach, where a road parallels the beach, together with a caravan park and the Christies Beach Surf Life Saving Club. A seawall protects the road, with a ramp to the beach in front of the surf club. Christies Creek flows across the middle of the beach and separates Christies Beach from O Sullivan Beach. The northern sewer works are fronted by a low sand dune, with the breakwater of a boat launching harbour forming the northern boundary. Both beaches receive low ocean swell as well as gulf wind waves, with waves averaging 0.5 to 1 m. This is sufficient to produce a single bar, usually cut by rips every 200 m. The centre of Christies Beach, where the surf club is located, is partly protected by Horseshoe Reef, which lies 300 m offshore. This causes the beach to protrude seaward at this point and receive slightly lower waves Swimming: This is a moderately hazardous beach owing to the common occurrence of rips. The safest swimming is right in front of the surf club, where the waves are usually a little lower and the beach is patrolled in summer. Watch out for rips and stay inshore on the attached portion of the bar. Surfing: This is a popular surfing beach owing to the low ocean swell that commonly reaches here. The swell, bars and rips can produce some reasonable beach breaks. Fishing: The rips produce holes for beach fishing, while there is also rock fishing off the southern Witton Bluff or the northern breakwater. However most fishers use the boat ramp to fish the outer reefs and gulf waters. Summary: A popular beach with some surf and good access and facilities. SOUTH PORT SLSC Patrols: November to March, weekends and public holidays. South Port Surf Life Saving Club patrols the southern 1 km of the 2 km long beach that includes Port Noarlunga Beach The southern section consists of the beach and sand dunes extending up to 200 m inland and then the meandering Onkaparinga River. The river flows out across the very southern end of the beach, against the bluffs and rock flats of Robinson Point. A road parallels the eastern side of the river. To reach the beach requires parking on the main road and walking across a footbridge and the dune, a total distance of 300 m. The surf club is located in the sand dunes 400 m north of the river mouth.

7 South Port Beach faces almost due west and receives low ocean swell, as well as gulf wind waves. Waves average 0.5 to 1 m and during higher wave conditions produce a double bar system, with three to four rips cutting across the inner and outer bars. During normal low wave conditions, the inner rips tend to infill and a continuous bar is attached to the beach. In addition, the river flows across the southern end of the beach building out a large tidal sand bar, cut by the deeper tidal channel. Swimming: South Port is one of the potentially more energetic of the Adelaide beaches and care should be taken here as rip channels and currents are common. Even during low waves the deeper rip channels may persist. Stay in the patrolled area and clear of the southern tidal channels and any rip holes. Surfing: The more exposed location makes South Port one of the more persistent surfing beaches, with low to moderate waves (0.5 to 1 m) breaking over both the inner and outer bars. Fishing: This is a popular spot with a choice of river, inlet, rock and beach fishing, the latter often into rip gutters and holes. Summary: A relatively natural beach and river mouth, with a more variable surf zone and a chance of bigger waves. MOANA SLSC Patrols: November to March, weekends and public Holidays The beach is relatively wide and flat, with an attached shallow bar, then a trough separating it from a shallow outer bar, the shape of which depends on wave conditions and at times has deep rip channels. Moana receives low swell and westerly wind waves, with waves averaging 0.5 to 1 m. North of the main beach the bluffs gradually increase in height, reaching 20 m at Robinson Point, where reef flats also front the adjoining 2 km long beach that is wedged between the bluffs and the flats. A road runs along the top of the bluffs, with several sloping access tracks down to the narrow beach. Swimming: Moana is a moderately safe beach under normal conditions. However care should be taken if swimming in the trough or on the outer bar, as rip currents may be present. All currents and rips intensify when waves exceed 1 m. Robinson Point is unsuitable for swimming owing to the rock flats, though there are some tidal pools at low tide. Surfing: There are usually low breaks over the inner and outer bars, with higher swell producing a better break. Fishing: There are occasional rip holes, particularly following larger swell and rock fishing off Ochre and Robinson Points. Summary: A popular and accessible beach, which receives some swell and usually has a low surf.

8 MIDDLETON Unpatrolled At Middleton are the first bedrock outcrops to occur on the coast since Cape Banks 320 km to the southeast. The Middleton residential area backs the 10 m high bluffs, which provide views of both the long Middleton beach as well as the rock dominated Middleton Rocks beach. A sealed road runs along the back of Middleton Rocks beach and the eastern end of Basham Beach, while access to Crockery Bay is from a car park located 300 m west of the beach. Middleton Rocks beach is dominated by dipping metasedimentary rocks which both border and front much of the 400 m long beach, with a central 30 m area clear of rock providing access to the ocean. Waves break across the rock reefs and a permanent rip flows out in front of the sand pocket. There is a car park at the western end of the beach, as well as the car park and facilities on Middleton Point at the eastern end. Swimming: Both Middleton Rocks and Crockery Bay beaches are dominated by rocks and are usually unsuitable for swimming. The eastern end of Basham, away from the rocks, offers the safest swimming area. Surfing: There is no recognised surf at any of these three beaches, although surfers do paddle out from Middleton Rocks during big seas to surf the adjoining Middleton beach breaks. Fishing: The rocks of Middleton Rocks and Commodore Point are the best locations. However, beware of large waves which wash over the rocks. Summary: Three accessible beaches with no facilities. WAITPINGA, PARSONS Unpatrolled Waitpinga Beach is one of the more popular surfing beaches on the Fleurieu Peninsula. It is located 15 km west of Victor Harbor, with a 3 km long sealed road leading from the main road right to the beach. There is a car park behind the dune and an elevated walkway across the dune to the centre of the 3.1 km long beach. The beach is backed by largely vegetated dunes, with Waitpinga Creek and its elongated lagoon behind the centre of the beach. A second parking area is located on the western headland, reached via Parsons Beach Road. The beach faces almost due south, exposing it to persistent high swell which averages about 2 m. Ninety metre high Newland Head forms the eastern boundary, with 40 m high Waitpinga Hill separating it from adjoining Parsons Beach. The combination of high swell and medium sand produces a steep beach and a surf zone dominated by eight to ten large rips, separated by bars which are usually detached from the beach. The alternating bars and rips produce megacusps, large scallops in the beach in lee of the rips and protrusions in lee of the bars. Strong permanent rips run out against each headland, in addition to rocks in the surf for 300 m south of Newland Head.

9 Parsons Beach, also known as Pareena Beach, lies immediately west of Waitpinga Hill headland and shares a cliff top car park with Waitpinga. There is a walking track from the car park down to the eastern end of the 1.2 km long beach. It receives moderate to high waves, which maintain a 150 m wide surf zone dominated by two permanent rips at either end and one to two central beach rips. Climbing vegetated dunes back the beach, with a small creek draining across the western end. Apart from the car park there are no facilities. Swimming: These are two exposed, usually high wave and always rip dominated beaches. There are deep rip channels and strong rip currents right off the beach. Only swim or surf here if you really know what you are doing and are a very experienced surfer. Surfing: The alternating rips and bars on Waitpinga produce a series of beach breaks which can hold good waves up to 3 m, while Parsons can hold up to about 2 m. However only surf with friends as conditions here can be very hazardous. Fishing: Waitpinga is a very popular spot for beach fishing owing to the deep, persistent rip gutters and holes, together with the rocks at each end. Summary: Two relatively natural and wild beaches backed by rising dunes and a central small lagoon at Waitpinga, and both fronted by the rip dominated surf. They are only suited for experienced surfers, otherwise it is worth the drive out for the view and a walk along the beach. VICTOR HARBOR Unpatrolled Victor Harbor beach is a 1 km long, curving, south facing beach, which usually receives waves averaging about 0.5 m. The entire beach is backed by a foreshore reserve and car parking, then the town of Victor Harbor. The beach usually has low to no surf, with the seagrass growing right to the beach. Swimming: These are four low energy and relatively safe beaches. The most popular are Victor Harbor and the Inman River mouth beaches, which are both backed by large reserves. Surfing: None in the bay, except during big seas when waves break at Victor Harbor beach. Fishing: The Rosetta Head wharf is the most popular shore based spot to fish from, along with the Inman River, particularly when the mouth is open. Summary: Four beaches set in a low energy bay, with excellent access to all and the facilities of Victor Harbor right behind.

Surfers Against Sewage Are Calling For A Review of the UK s Bathing Water Sample Sites.

Surfers Against Sewage Are Calling For A Review of the UK s Bathing Water Sample Sites. Surfers Against Sewage Are Calling For A Review of the UK s Bathing Water Sample Sites. Welsh Report Surfers Against Sewage (SAS) believe the weekly bathing water samples required by the EU Bathing Water

More information

Beach 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 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 information

LAB: WHERE S THE BEACH

LAB: 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 information

There are many different kinds of beaches which are generally characterized by the dominance of waves, tides, rivers and currents, and in particular

There 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 information

Reading Material. Inshore oceanography, Anikouchine and Sternberg The World Ocean, Prentice-Hall

Reading 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 information

Anatomy of Coastal Regions

Anatomy 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 information

Chapter 10 Lecture Outline. The Restless Oceans

Chapter 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 information

Shorelines Earth - Chapter 20 Stan Hatfield Southwestern Illinois College

Shorelines 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 information

General Water Safety Tips

General Water Safety Tips General Wherever there is water these rules apply. Know the Aquacode Go Together, Stay Afloat and Wave, Reach to Rescue. Always swim with a friend or adult. To reach and rescue, lie down and stretch out.

More information

Marginal Marine Environments

Marginal 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 information

Montessori for Everyone 2013 Types of Coastlines

Montessori for Everyone 2013 Types of Coastlines 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

More information

Overview. Beach Features. Coastal Regions. Other Beach Profile Features. CHAPTER 10 The Coast: Beaches and Shoreline Processes.

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 information

Wave-dominated embayed beaches. Andrew D Short School of Geosciences University of Sydney

Wave-dominated embayed beaches. Andrew D Short School of Geosciences University of Sydney Wave-dominated embayed beaches Andrew D Short School of Geosciences University of Sydney Wave-dominated embayed beaches wave-dominated beaches embayed beaches morphodynamics of W-D embayed beaches circulation,

More information

Oceans and Coasts. Chapter 18

Oceans 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 information

2007 Encounter Bay Whale Sighting Log DATE TIME LOCATION GRID REF DISTANCE FROM SHORE ADULT CALF/JUVENILE SPECIES BEHAVIOUR COMMENTS

2007 Encounter Bay Whale Sighting Log DATE TIME LOCATION GRID REF DISTANCE FROM SHORE ADULT CALF/JUVENILE SPECIES BEHAVIOUR COMMENTS 2007 Encounter Bay Sighting Log DATE TIME LOCATION GRID REF DISTANCE FROM SHORE ADULT CALF/JUVENILE SPECIES BEHAVIOUR COMMENTS 20/09/07 10.30am Between King's Beach and the Bluff, N/A 50 metres 1 Southern

More information

Delaware Chapter Surfrider Foundation - Indian River Inlet Monitoring

Delaware Chapter Surfrider Foundation - Indian River Inlet Monitoring Delaware Chapter Surfrider Foundation - Indian River Inlet Monitoring In 2012, the Delaware Surfrider Foundation Chapter formed the Surf Quality and Access Committee to focus on issues such as surf spot

More information

1.5 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) 1.5 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 information

HARBOUR SEDIMENTATION - COMPARISON WITH MODEL

HARBOUR SEDIMENTATION - COMPARISON WITH MODEL HARBOUR SEDIMENTATION - COMPARISON WITH MODEL ABSTRACT A mobile-bed model study of Pointe Sapin Harbour, in the Gulf of St. Lawrence, resulted in construction of a detached breakwater and sand trap to

More information

Essentials of Oceanography Eleventh Edition

Essentials 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 information

OECS Regional Engineering Workshop September 29 October 3, 2014

OECS Regional Engineering Workshop September 29 October 3, 2014 B E A C H E S. M A R I N A S. D E S I G N. C O N S T R U C T I O N. OECS Regional Engineering Workshop September 29 October 3, 2014 Coastal Erosion and Sea Defense: Introduction to Coastal Dynamics David

More information

COASTAL ENVIRONMENTS. 454 lecture 12

COASTAL 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 information

The Case of the Disappearing Shoreline

The 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 information

Beaches Unit (4.5 pts)

Beaches 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 information

Impacts of breakwaters and training walls

Impacts 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

Port Stephens Council

Port Stephens Council Port Stephens ouncil State of the eaches 22 23 Overall results Percentage of sites graded as Good or Good: 9 Nine of the eleven swimming sites were graded as Good or Good in 22 23, a fall in performance

More information

A full version of this guide is available with photos online at

A full version of this guide is available with photos online at Llyn.info Beach Guide Printable version to take with you the use of any information on Llyn.info is at the risk of the user and Llyn.info, it s webmaster nor any of it s advertisers can be held responsible

More information

Australian Coastal Councils Conference

Australian Coastal Councils Conference Australian Coastal Councils Conference Kiama March 2019 Where Has My Beach Gone? (and what can I do about it?) Dr Andrew McCowan Water Technology Where Has My Beach Gone? Where Has My Beach Gone? Where

More information

1.5 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) 1.5 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 information

Risk Assessment. Compiled by: Lawrence Smith Date Compiled: 1 February 2009

Risk Assessment. Compiled by: Lawrence Smith Date Compiled: 1 February 2009 Risk Assessment Compiled by: Lawrence Smith Date Compiled: 1 February 2009 Location: Gwithian Date of Activity: Ongoing Activity: Kitesurfing on the sea and launching and landing of LEI kites on land.

More information

Earth Science Chapter 16 Section 3 Review

Earth 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 information

Environmental Protection on the Gold Coast of Queensland, Australia. 1. What is the appeal of the Gold Coast to tourists?

Environmental Protection on the Gold Coast of Queensland, Australia. 1. What is the appeal of the Gold Coast to tourists? Environmental Protection on the Gold Coast of Queensland, Australia Sections 1. What is the appeal of the Gold Coast to tourists? 2. How are Gold Coast visitor trends changing? 3. How can the impacts of

More information

Chesil Beach, Dorset UK High energy, shingle coastline. Brighton Beach, Sussex UK Pebble beach

Chesil 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 information

Volume and Shoreline Changes along Pinellas County Beaches during Tropical Storm Debby

Volume and Shoreline Changes along Pinellas County Beaches during Tropical Storm Debby Volume and Shoreline Changes along Pinellas County Beaches during Tropical Storm Debby Ping Wang and Tiffany M. Roberts Coastal Research Laboratory University of South Florida July 24, 2012 Introduction

More information

Thank you for signing up to the 30 Bays in 30 Days Challenge!

Thank you for signing up to the 30 Bays in 30 Days Challenge! Introduction Thank you for signing up to the 30 Bays in 30 Days Challenge! The challenge takes place in July when everyone is invited to swim in 30 bays throughout the month. It s a fantastic way to explore

More information

WALLAROO AND ENVIRONS VENUES FOR 2015 NATIONAL CARNIVAL AND ANGLING CHAMPIONSHIPS

WALLAROO AND ENVIRONS VENUES FOR 2015 NATIONAL CARNIVAL AND ANGLING CHAMPIONSHIPS WALLAROO AND ENVIRONS VENUES FOR 2015 NATIONAL CARNIVAL AND ANGLING CHAMPIONSHIPS Map of AAA 2015 National Angling Championships Area Venue. Note it is 2 hours drive from Adelaide. The following are a

More information

MAR 110 LECTURE #15 Wave Hazards

MAR 110 LECTURE #15 Wave Hazards 1 MAR 110 LECTURE #15 Wave Hazards Rogue Wave Hazard Rogue waves are very large open ocean waves of sometimes can range in height from 60 ft (20m) to120 feet (40m) and thus a significant hazard to large

More information

Apostle Islands National Seashore

Apostle Islands National Seashore Apostle Islands National Seashore David Speer & Phillip Larson October 2 nd Fieldtrip Report Table of Contents Introduction 1 Stop 1: Apostle Island Boat Cruise 1 Stop 2: Coastal Geomorphology 5 Stop 3:

More information

HIGHVIEW COLLEGE RECREATIONAL WATER POLICY

HIGHVIEW COLLEGE RECREATIONAL WATER POLICY HIGHVIEW COLLEGE RECREATIONAL WATER POLICY Person Responsible Sports Co-ordinator Rationale Recreational swimming occurs when learning swimming and water safety is not the main objective of the activity.

More information

Chapter. The Dynamic Ocean

Chapter. 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 information

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,

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, 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 information

General Coastal Notes + Landforms! 1

General 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 information

Lecture Outlines PowerPoint. Chapter 15 Earth Science, 12e Tarbuck/Lutgens

Lecture 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 information

Chapter 12: Coasts (after a brief review of Tides)

Chapter 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 information

Shore - place where ocean meets land Coast - refers to the larger zone affected by the processes that occur at this boundary.

Shore - 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 information

Shoreline Response to an Offshore Wave Screen, Blairgowrie Safe Boat Harbour, Victoria, Australia

Shoreline Response to an Offshore Wave Screen, Blairgowrie Safe Boat Harbour, Victoria, Australia Shoreline Response to an Offshore Wave Screen, Blairgowrie Safe Boat Harbour, Victoria, Australia T.R. Atkins and R. Mocke Maritime Group, Sinclair Knight Merz, P.O. Box H615, Perth 6001, Australia ABSTRACT

More information

Deep-water orbital waves

Deep-water orbital waves What happens when waves approach shore? Deep-water orbital waves Fig. 9.16, p. 211 Wave motion is influenced by water depth and shape of the shoreline wave buildup zone surf zone beach Wave base deepwater

More information

Figure 1. Schematic illustration of the major environments on Mustang Island.

Figure 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 information

Chapter 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 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 information

Natural Bridges Field Trip Activity

Natural Bridges Field Trip Activity Natural Bridges Field Trip Activity This is due in class on MONDAY- March 1 - not in sections! Name TA: NOTE ON THE GRADING OF THIS ASSIGNMENT: Many of the questions below (especially in the tidepool part)

More information

RI Regulatory Setbacks & Buffers: Coastal Management Issues

RI Regulatory Setbacks & Buffers: Coastal Management Issues RI Regulatory Setbacks & Buffers: Coastal Management Issues New England Onsite Wastewater Training Program @ URI OWT 155 - November 29, 2012 James Boyd - Coastal Policy Analyst Photo: October 30, 2012

More information

BEACH PROCESSES AND COASTAL ENVIRONMENTS

BEACH 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 information

Nearshore Sediment Transport What influences the loss of sediment on Beaches? - Waves - Winds - Tidal Currents - River discharge - Runoff

Nearshore 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 information

The Sea Geography Notes JC-Learn. JC-Learn. Geography Notes The Sea. 1 P a g e

The 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 information

For more information: Photography: Rijkswaterstaat (Leo Linnartz, Carrie de Wilde, Jurriaan Brobbel, Joop van Houdt), Deltares

For more information: Photography: Rijkswaterstaat (Leo Linnartz, Carrie de Wilde, Jurriaan Brobbel, Joop van Houdt), Deltares Investing in your future. This project was made possible with support from the European Regional Development Fund. Photography: Rijkswaterstaat (Leo Linnartz, Carrie de Wilde, Jurriaan Brobbel, Joop van

More information

page - Laboratory Exercise #5 Shoreline Processes

page - 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 information

Nearshore Morphodynamics. Bars and Nearshore Bathymetry. Sediment packages parallel to shore, that store beach sediment

Nearshore Morphodynamics. Bars and Nearshore Bathymetry. Sediment packages parallel to shore, that store beach sediment Nearshore Morphodynamics http://coastal.er.usgs.gov/bier/images/chandeleur-xbeach-lg.jpg Bars and Nearshore Bathymetry Sediment packages parallel to shore, that store beach sediment Can be up to 50 km

More information

4/20/17. #30 - Coastlines - General Principles Coastlines - Overview

4/20/17. #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 information

Upstreampaddle 25.South arm of the Brunswick River, Simpson s Creek drains the freshwater swamp lands of Tyagarah Nature Reserve, 750 hectares. Furthe

Upstreampaddle 25.South arm of the Brunswick River, Simpson s Creek drains the freshwater swamp lands of Tyagarah Nature Reserve, 750 hectares. Furthe Upstreampaddle 24 The Brunswick River is a shorter length river on the coastal plain of Northern New South Wales. The areas of interest to canoeists are: the reach from the town of Mullumbimby down to

More information

Coastal management has lagged behind the growth in population leading to problems with pollution

Coastal 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 information

TITLE: COASTAL EROSION AND LANDFORMS.

TITLE: 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 information

Thank you for signing up to the 30 Bays in 30 Days Challenge!

Thank you for signing up to the 30 Bays in 30 Days Challenge! Introduction Thank you for signing up to the 30 Bays in 30 Days Challenge! The challenge takes place in July when everyone is invited to swim in 30 bays throughout the month. It s a fantastic way to explore

More information

Coasts. 1. Coastal Processes. 1.1 Coastal erosion. 1.2 Sediment transport. Coastal Processes and Landforms. i. Hydraulic action

Coasts. 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 information

Warm-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 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 information

Red Rocks Pari-whero. Red Rocks/Pari-Whero. Quarry. Owhiro Bay Quarry. Owhiro Bay Parade. Taputeranga Marine Reserve ISSUES AND OPPORTUNITIES ANALYSIS

Red Rocks Pari-whero. Red Rocks/Pari-Whero. Quarry. Owhiro Bay Quarry. Owhiro Bay Parade. Taputeranga Marine Reserve ISSUES AND OPPORTUNITIES ANALYSIS Red Rocks Pari-whero Wild coastal environment Shared path with WD vehicles Red Rocks/Pari-Whero Owhiro Bay Parade Owhiro Bay Quarry Quarry Taputeranga Marine Reserve 2 PART Potential future links Makara

More information

Monterey Peninsula College

Monterey 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 information

Environmental Definitions and Deployment Guidance for Instructors, Coaches and Leaders

Environmental Definitions and Deployment Guidance for Instructors, Coaches and Leaders Environmental s and Deployment Guidance for Instructors, Coaches and Leaders This document provides guidance and environmental definitions that can be applied when choosing paddlesport activity. British

More information

Läna 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 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 information

Habitat Fact Sheets. Rocky habitats are dominated by seaweeds and often mussels, which rely on the rocks for attachment.

Habitat Fact Sheets. Rocky habitats are dominated by seaweeds and often mussels, which rely on the rocks for attachment. Habitat Fact Sheets Habitats in the Gulf of Maine serve many important roles for the environment and for humans as well. These include: cycling nutrients, filtering pollution, trapping sediments, storing

More information

West Coast Anchorages

West Coast Anchorages West Coast Anchorages This document aims to catalogue a number of anchorages along the West Coast of Tasmania where shelter may be sought. In addition the degree of protection from the wind, and holding

More information

Map 8: Ayrshire Coast: Ardrossan North Bay to Stevenston Pier Map Content Descriptions

Map 8: Ayrshire Coast: Ardrossan North Bay to Stevenston Pier Map Content Descriptions Map 8: Ayrshire Coast: Ardrossan North Bay to Stevenston Pier Map Content Descriptions 1. Built Heritage and Archaeology A total of twenty four sites were recorded in the area covered by Map 8. Of these

More information

GONE! Coastal Erosion Happens During Storms! Why Worry About Coastal Setbacks? Goals for Today

GONE! Coastal Erosion Happens During Storms! Why Worry About Coastal Setbacks? Goals for Today RI Regulatory Setbacks & Buffers: Coastal Zone Management Issues New England Onsite Wastewater Training Program @ URI OWT 155 November 21, 2013 Goals for Today Understand the impacts of storms, coastal

More information

Formation and characteristics of different types of beaches

Formation 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 information

Cymyran Strait and Rhoscolyn

Cymyran Strait and Rhoscolyn Borthwen and Rhoscolyn Beacon - Photo: www.pixaerial.com 7 No. 7 Grade B 18km OS Sheet 114 Tidal Port Liverpool Start Four Mile Bridge (280783) Finish Porth Dafarch (233800) HW/LW are around 1 hour 30

More information

ATLANTIC COUNTY 2006 to 2008

ATLANTIC COUNTY 2006 to 2008 ATLANTIC COUNTY 2006 to 2008 The Atlantic County oceanfront shoreline consists of three barrier islands where the northern one, Little Beach Island and a third of the second, Brigantine Island, are undeveloped

More information

Estuarine Shoreline Stabilization

Estuarine 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 information

Low-crested offshore breakwaters: a functional tool for beach management

Low-crested offshore breakwaters: a functional tool for beach management Environmental Problems in Coastal Regions VI 237 Low-crested offshore breakwaters: a functional tool for beach management K. Spyropoulos & E. Andrianis TRITON Consulting Engineers, Greece Abstract Beach

More information

DUNE STABILIZATION AND BEACH EROSION

DUNE STABILIZATION AND BEACH EROSION DUNE STABILIZATION AND BEACH EROSION CAPE HATTERAS NATIONAL SEASHORE NORTH CAROLINA ROBERT DOLAN PAUL GODFREY U. S. DEPARTMENT OF INTERIOR NATIONAL PARK SERVICE OFFICE OF NATURAL SCIENCE WASHINGTON, D.

More information

Coastal Processes Day Criccieth

Coastal 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 information

General Information on Drowning

General Information on Drowning General Information on Drowning Drowning is the third leading cause of accidental death in the United States and the second leading cause of accidental death for persons aged 5 to 44. For children in the

More information

* Appalachian Mountains -the mountain range in the Eastern U.S. which terminates in north-central Alabama

* Appalachian Mountains -the mountain range in the Eastern U.S. which terminates in north-central Alabama MR. SAND TEACHER'S MANUAL INTRODUCTION: Although Mr. Sand is a cartoon presentation that is attractive to children (of all ages), the material is technically accurate and quite significant to our understanding

More information

Dynamic Shoreline. Why do we care? Loss of land Damage to structures Recreation

Dynamic Shoreline. Why do we care? Loss of land Damage to structures Recreation Dynamic Shoreline Why do we care? Loss of land Damage to structures Recreation Coastal Water Movement Waves provide the energy Through breaking As waves shoal Speed decreases Height increases Wavelength

More information

Wallarah Coastal Walk

Wallarah Coastal Walk Wallarah Coastal Walk 3 hrs 8.3 km Return Hard track 247m This walk starts at Caves Beach and travels south along the coastline, until reaching the Pinney s Headland Lookout. There are many opportunities

More information

Montserrat. Wise practices for coping with. i b bea n Se a

Montserrat. Wise practices for coping with. i b bea n Se a Wise practices for coping with Montserrat Car i b bea n Se a Fisheries Division, Montserrat Physical Planning Department, Montserrat University of Puerto Rico, Sea Grant College Program Caribbean Development

More information

CHAPTER 134 INTRODUCTION

CHAPTER 134 INTRODUCTION CHAPTER 134 NEW JETTIES FOR TUNG-KANG FISHING HARBOR, TAIWAN Chi-Fu Su Manager Engineering Department Taiwan Fisheries Consultants, Inc. Taipei, Taiwan INTRODUCTION Tung-Kang Fishing Harbor, which is about

More information

Oceans in Motion: Waves and Tides

Oceans in Motion: Waves and Tides Oceans in Motion: Waves and Tides Waves Waves are among the most familiar features in the ocean. All waves work similarly, so although we are talking about ocean waves here, the same information would

More information

SANDBANKS COAST PROTECTION

SANDBANKS COAST PROTECTION SANDBANKS COAST PROTECTION David Robson, Senior Engineer, Coastal & Drainage Team Borough of Poole Leisure Services (T) 01202 265265 (E) d.robson@poole.gov.uk May 2003 SANDBANKS COAST PROTECTION Introduction

More information

COASTAL SYSTEMS WAVE ENERGY

COASTAL 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 information

Julebæk Strand. Effect full beach nourishment

Julebæk Strand. Effect full beach nourishment Julebæk Strand Effect full beach nourishment Aim of Study This study is a part of the COADAPT funding and the aim of the study is to analyze the effect of beach nourishment. In order to investigate the

More information

Rip Current Rip Tide,

Rip Current Rip Tide, Rip Current A Rip Current, sometimes called a Rip Tide, is one specific kind of water current that can be found near beaches. It is a strong, localized, narrow current of water. It is strongest near the

More information

Wave, Tide or Ride, Follow the Guide

Wave, Tide or Ride, Follow the Guide Wave, Tide or Ride, Follow the Guide KEY TERMS Catch pool: A landing pool located at the bottom of a water slide. Current: The continuous movement of water. Dispatcher: The lifeguard at the top of a water

More information

SPECIAL SPRING 2018 STORM REPORT ON THE CONDITION OF THE MUNICIPAL BEACHES FOR THE BOROUGH OF STONE HARBOR, CAPE MAY COUNTY, NEW JERSEY

SPECIAL SPRING 2018 STORM REPORT ON THE CONDITION OF THE MUNICIPAL BEACHES FOR THE BOROUGH OF STONE HARBOR, CAPE MAY COUNTY, NEW JERSEY SPECIAL SPRING 2018 STORM REPORT ON THE CONDITION OF THE MUNICIPAL BEACHES FOR THE BOROUGH OF STONE HARBOR, CAPE MAY COUNTY, NEW JERSEY Aerial photograph taken April 21, 2018 showing the view up the beach

More information

RAINBOW BAY FIELD REPORT

RAINBOW BAY FIELD REPORT RAINBOW BAY FIELD REPORT Contents Page Abstract 1.0 Introduction.. 2.0 Methodology 2.1 Limitations.. 3.0 Statement of Findings. 3.1 History. 3.2 Data Collection. 3.2.1 Observations. 3.2.2 Management Strategies

More information

Controlling Coastal erosion

Controlling 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 information

STATUS REPORT FOR THE SUBMERGED REEF BALL TM ARTIFICIAL REEF SUBMERGED BREAKWATER BEACH STABILIZATION PROJECT FOR THE GRAND CAYMAN MARRIOTT HOTEL

STATUS REPORT FOR THE SUBMERGED REEF BALL TM ARTIFICIAL REEF SUBMERGED BREAKWATER BEACH STABILIZATION PROJECT FOR THE GRAND CAYMAN MARRIOTT HOTEL August 23 STATUS REPORT FOR THE SUBMERGED REEF BALL TM ARTIFICIAL REEF SUBMERGED BREAKWATER BEACH STABILIZATION PROJECT FOR THE GRAND CAYMAN MARRIOTT HOTEL performed by Lee E. Harris, Ph.D., P.E. Consulting

More information

Figure 1, Chart showing the location of the Breach at Old Inlet and sensors deployed in Great South Bay.

Figure 1, Chart showing the location of the Breach at Old Inlet and sensors deployed in Great South Bay. The Impact on Great South Bay of the Breach at Old Inlet Charles N. Flagg and Roger Flood School of Marine and Atmospheric Sciences, Stony Brook University The Great South Bay project (http://po.msrc.sunysb.edu/gsb/)

More information

CORPS FACTS. Harbor Dredging U.S. ARMY CORPS OF ENGINEERS BUILDING STRONG

CORPS FACTS. Harbor Dredging U.S. ARMY CORPS OF ENGINEERS BUILDING STRONG CORPS FACTS Harbor Dredging U.S. ARMY CORPS OF ENGINEERS BUILDING STRONG Disaster Response Sedimentation in the channel is caused by the normal cycle of silt movement, erosion from high water or heavy

More information

Visiting Lake Macquarie

Visiting Lake Macquarie Visiting Lake Macquarie Lake Macquarie is the largest coastal salt water lake in Australia and is a prime boating destination for both small and large vessels. Many sailing regattas and fishing activities

More information

Cove Point Beach Restoration: Utilization of a Spawning Habitat by Horseshoe Crabs (Limulus polyphemus)

Cove Point Beach Restoration: Utilization of a Spawning Habitat by Horseshoe Crabs (Limulus polyphemus) Cove Point Beach Restoration: Utilization of a Spawning Habitat by Horseshoe Crabs (Limulus polyphemus) Paul Bushmann, Jessica Peterson, Bethany Enyeart and Deborah Smith Anne Arundel Community College

More information

4 th Quarter 2014 Report OC MPA Watch Program Orange County Coastkeeper

4 th Quarter 2014 Report OC MPA Watch Program Orange County Coastkeeper 4 th Quarter 2014 Report OC MPA Watch Program Orange County Coastkeeper Intro January 1 st, 2012 was the implementation date for the South Coast MPAs from Point Conception to the Mexican border. The Orange

More information

Species Conclusions Table

Species Conclusions Table Conclusions Table Project Name: Chesapeake Landing HOA- Breakwaters (NAO-14-0283) Date: February 25, 2014 /Resource Name Loggerhead sea turtle (Caretta caretta) Conclusion ESA Section 7 / Eagle Act Determination

More information