WThis is a list of the units into which the rock succession of New Zealand is formally divided. As new geological relationships have been discovered new names have been proposed and others are made obsolete. Not all these changes have been universally adopted. This table is based on the 2014 New Zealand Stratigraphic Lexicon (Litho2014). However, obsolete names that are still in use and names postdating the lexicon are included if it aids in understanding.
WThe Boulder Bank is a very unusual naturally formed landform in Nelson, New Zealand. It is a 13 kilometre long stretch of rocky substrate which begins at the Mackay Bluff and ends at the Cut of the Nelson Harbour. Haulashore Island was once a part of the Boulder Bank, but the Cut made it an island, and it is no longer connected to the Boulder Bank. The Boulder Bank separates Tasman Bay and the Nelson Haven and is managed as a scenic reserve by the Department of Conservation. Land access is gained along Boulder Bank Drive, signposted at the northern end of Nelson Haven on State Highway 6.
WCape Kidnappers / Te Kauwae-a-Māui is a headland at the southeastern extremity of Hawke's Bay on the east coast of New Zealand's North Island and sits at the end of an 8 kilometres (5.0 mi) peninsula which protrudes into the Pacific Ocean. It is 20 kilometres (12 mi) south-east of the city of Napier. Access to the Cape by road stops at Clifton, which is the departure point for many tourists. The Cape Kidnappers Golf Course lies between the headland and the nearby coastal community of Te Awanga.
WCurio Bay is a coastal embayment in the Southland District of New Zealand, best known as the site of a petrified forest some 180 million years old. It also hosts a yellow-eyed penguin colony, arguably the rarest of penguin species, with approximately 1600 breeding pairs in the extant population. The bay, along with neighbouring Porpoise Bay, is home to the endemic Hector's dolphin. Southern right whales are occasionally observed offshore, as on numerous parts of the country's coast. Located near the southernmost point of the South Island, Curio Bay is one of the major attractions in the Catlins, attracting around 100,000 visitors per year. The town of Waikawa has an information center for tourists.
WKupe's Sail is a geological formation near the eastern end of Palliser Bay at the southern end of the North Island of New Zealand.
WPiha is a coastal settlement 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.
WThe Oparara Basin Arches are a number of natural limestone tunnels formed by the Oparara River, in the Oparara Basin, New Zealand. The two most famous ones are the 'Oparara Arch', large enough for a multi-storey house, and the 'Moria Gate Arch', which is smaller in height.
WPunakaiki is a small community on the West Coast of the South Island of New Zealand, between Westport and Greymouth. The community lies on the edge of the Paparoa National Park.
WThe Pink Terrace, or Te Otukapuarangi in Māori, and the White Terrace, also known as Te Tarata, were natural wonders of New Zealand. They were reportedly the largest silica sinter deposits on earth. Until recently, they were lost and thought destroyed in the 1886 eruption of Mount Tarawera, while new hydrothermal features formed to the south-west i.e. Waimangu Volcanic Rift Valley.
WThe Putangirua Pinnacles are a geological formation and one of New Zealand's best examples of badlands erosion. They consist of a large number of earth pillars or hoodoos located at the head of a valley in the Aorangi Ranges, on the North Island of New Zealand, in the Wellington region.
WTe Paepae o Aotea, also known the Volkner Rocks, are a group of andesitic rock stacks and pinnacles located 5 kilometres (3.1 mi) northwest of Whakaari/White Island in New Zealand's Bay of Plenty. They reach 113 metres above sea level, while the saddle separating them from Whakaari/White Island is over 200 metres deep.