Hot Water Beach is a beach on the east coast of the Coromandel Peninsula, New Zealand, just south of Mercury Bay. [1] It is approximately 12 kilometres south east of Whitianga, and approximately 175 kilometres from Auckland by car. Its name comes from underground hot springs that filter up through the sand between the high and low water tidal reaches. The beach is a popular destination both for locals and tourists visiting New Zealand. Annual visitor numbers have been estimated at 700,000, making it one of the most popular geothermal attractions in the Waikato region. [2]
Within two hours either side of low tide, it is possible to dig into the sand allowing hot water to escape to the surface forming a hot water pool. The water, with a temperature as hot as 64 °C (147 °F), filters up from two underground fissures located close to each other. [1] These natural springs can be found on the beach opposite the off-shore rocks. Visitors often dig large holes and relax and soak in the thermal water. Many visitors bring a spade and bucket with them. Spades can also be hired from the nearby surf shop. [3]
Care needs to be exercised as the location of the hot springs are not far from the sea even at low tide, and visitors may be caught unaware by the large breaking waves. Hot Water Beach is known for its dangerous rip currents, holes and large waves. Signs at the beach advise swimmers not to swim within 50 m either side of the off-shore rocks (opposite the springs), and to only swim between the flags of the Hot Water Beach Lifeguard Service. [4] Hot Water Beach's rip currents have claimed the lives of several unwary visitors and only strong and experienced swimmers are advised to enter the water.
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material.
The Tidal River is a perennial river of the West Gippsland catchment, located in the Wilsons Promontory region of the Australian state of Victoria. A permanent camping ground which the river flows passed to the south is also called Tidal River.
A rip current is a specific type of water current that can occur near beaches where waves break. A rip is a strong, localized, and narrow current of water that moves directly away from the shore by cutting through the lines of breaking waves, like a river flowing out to sea. The force of the current in a rip is strongest and fastest next to the surface of the water.
A rip tide, or riptide, is a strong offshore current that is caused by the tide pulling water through an inlet along a barrier beach, at a lagoon or inland marina where tide water flows steadily out to sea during ebb tide. It is a strong tidal flow of water within estuaries and other enclosed tidal areas. The riptides become the strongest where the flow is constricted. When there is a falling or ebbing tide, the outflow water is strongly flowing through an inlet toward the sea, especially once stabilized by jetties.
A lifeguard is a rescuer who supervises the safety and rescue of swimmers, surfers, and other water sports participants such as in a swimming pool, water park, beach, spa, river and lake. Lifeguards are trained in swimming and CPR/AED first aid, certified in water rescue using a variety of aids and equipment depending on requirements of their particular venue. In some areas, lifeguards are part of the emergency services system to incidents and in some communities, lifeguards may function as the primary EMS provider.
Piha is a coastal settlement in West Auckland, on the western coast of the Auckland Region in New Zealand. It is one of the most popular beaches in the area and a major day-trip destination for Aucklanders throughout the year, and especially in summer.
Huntington State Beach is a protected beach in Southern California, located in the City of Huntington Beach in Orange County. It extends 2 miles (3.2 km) from Newport Beach north to Beach Boulevard, where the Huntington City Beach begins. The 121-acre (49 ha) park was established in 1942.
Trebarwith Strand is a section of coastline located near the coastal settlement of Trebarwith on the north coast of Cornwall, England, UK, 2+1⁄2 miles (4.0 km) south of Tintagel. It has 800m of sandy beach contained by cliffs in which natural caves are found. The beach can only be accessed at low tide. The strand was once used to land ships to export slate from the nearby quarries while sand from the beach was used for agricultural purposes. The view from the beach is dominated by rocks 300m offshore known as Gull Rock or Otterham Rocks.
As ocean surface waves approach shore, they get taller and break, forming the foamy, bubbly surface called surf. The region of breaking waves defines the surf zone, or breaker zone. After breaking in the surf zone, the waves continue to move in, and they run up onto the sloping front of the beach, forming an uprush of water called swash. The water then runs back again as backwash. The nearshore zone where wave water comes onto the beach is the surf zone. The water in the surf zone is shallow, usually between 5 and 10 m deep; this causes the waves to be unstable.
Zuma Beach is a county beach at 30000 Pacific Coast Highway (PCH) in Malibu, California. One of the largest and most popular beaches in Los Angeles County, California, it is known for its long, wide sands and excellent surf. It consistently ranks among the healthiest beaches for clean water conditions in Los Angeles County.
The Auckland Region of New Zealand is built on a basement of greywacke rocks that form many of the islands in the Hauraki Gulf, the Hunua Ranges, and land south of Port Waikato. The Waitākere Ranges in the west are the remains of a large andesitic volcano, and Great Barrier Island was formed by the northern end of the Coromandel Volcanic Zone. The Auckland isthmus and North Shore are composed of Waitemata sandstone and mudstone, and portions of the Northland Allochthon extend as far south as Albany. Little Barrier Island was formed by a relatively isolated andesitic volcano, active around 1 to 3 million years ago.
A baïne is a pool of water of a few dozen to several hundred metres in length, parallel to the beach and directly connected to the sea. Each one is spaced every 300 to 400 metres and formed under the influence of waves and the tide. The French term baïne is typical for the Aquitaine coast of France in the departements of Gironde, Charente-Maritime and Landes, but it can occur on beaches throughout the world.
Praia do monte Clérigo is a beach within the municipality of Aljezur, in Algarve, Portugal. The beach is on the western Seaboard in the north west of the Algarve. The beach is 5.1 miles (8.2 km) north west of the village of Aljezur, and is 70.0 miles (112.7 km) north west, by road, from the regions capital of Faro. Praia do monte Clérigohas been designated a blue Flag beach (2012).
New Chums Beach is a beach in the Wainuiototo Bay on the northeast coast of the Coromandel Peninsula, New Zealand, near Whangapoua.
The Robberg Nature Reserve and Marine Protected Area is an inshore conservation region in the territorial waters of South Africa, near Plettenberg Bay in the Western Cape province.
The Browns Bank Complex Marine Protected Area is an offshore conservation region in the exclusive economic zone of South Africa
Tomahawk Beach is a beach on the Pacific Ocean 7.5 kilometres (4.7 mi) southeast of the city centre of Dunedin, New Zealand. Located within the Ocean Grove Reserve between St Kilda Beach and Smaills Beach, at the point where Otago Peninsula joins the mainland of the South Island, Tomahawk Beach is a white sand beach popular with casual beach-goers and dog-walkers as well as surfers. Sand is extracted from the Tomahawk Lagoon channel, which runs across the beach, for commercial purposes and to prevent flooding.
The Pancake Rocks and Blowholes are a coastal rock formation at Punakaiki on the West Coast of the South Island of New Zealand. They are a popular visitor attraction.