Wairere Boulders
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Wairere Boulders
Wairere Boulders is a privately-owned nature reserve and tourist attraction at Horeke in the south Hokianga region of Northland Region, Northland, New Zealand. The property contains geologically rare rock formations. Visitors to the property can walk around the various trails, kayak down the boulder river and stay at the campsite. Ownership Wairere Boulders was initially developed as a tourist attraction by Felix and Rita Schaad, a couple originally from Switzerland who owned the property from the 1980s. They opened the site for visitors in 2003, after 4 years work developing tracks, bridges and lookouts. The property was put up for sale in 2017. The property was purchased by Graham and Paula Grant, who are originally from Scotland. They have subsequently cut a new track, and added a camping site, a coffee caravan, and a bed and breakfast accommodation. The property includes farmland, and the owners raise miniature highland cattle. Visitor attractions The main attraction a ...
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Nonprofit Organization
A nonprofit organization (NPO) or non-profit organisation, also known as a non-business entity, not-for-profit organization, or nonprofit institution, is a legal entity organized and operated for a collective, public or social benefit, in contrast with an entity that operates as a business aiming to generate a Profit (accounting), profit for its owners. A nonprofit is subject to the non-distribution constraint: any revenues that exceed expenses must be committed to the organization's purpose, not taken by private parties. An array of organizations are nonprofit, including some political organizations, schools, business associations, churches, social clubs, and consumer cooperatives. Nonprofit entities may seek approval from governments to be Tax exemption, tax-exempt, and some may also qualify to receive tax-deductible contributions, but an entity may incorporate as a nonprofit entity without securing tax-exempt status. Key aspects of nonprofits are accountability, trustworth ...
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Hawaii
Hawaii ( ; haw, Hawaii or ) is a state in the Western United States, located in the Pacific Ocean about from the U.S. mainland. It is the only U.S. state outside North America, the only state that is an archipelago, and the only state geographically located within the tropics. Hawaii comprises nearly the entire Hawaiian archipelago, 137 volcanic islands spanning that are physiographically and ethnologically part of the Polynesian subregion of Oceania. The state's ocean coastline is consequently the fourth-longest in the U.S., at about . The eight main islands, from northwest to southeast, are Niihau, Kauai, Oahu, Molokai, Lānai, Kahoolawe, Maui, and Hawaii—the last of these, after which the state is named, is often called the "Big Island" or "Hawaii Island" to avoid confusion with the state or archipelago. The uninhabited Northwestern Hawaiian Islands make up most of the Papahānaumokuākea Marine National Monument, the United States' largest protected ...
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Rock Formations Of The Northland Region
Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales * Rock, Cornwall, a village in England * Rock, County Tyrone, a village in Northern Ireland * Rock, Devon, a location in England * Rock, Neath Port Talbot, a location in Wales * Rock, Northumberland, a village in England * Rock, Somerset, a location in Wales * Rock, West Sussex, a hamlet in Washington, England * Rock, Worcestershire, a village and civil parish in England United States * Rock, Kansas, an unincorporated community * Rock, Michigan, an unincorporated community * Rock, West Virginia, an unincorporated community * Rock, Rock County, Wisconsin, a town in southern Wisconsin * Rock, Wood County, Wisconsin, a town in central Wisconsin Elsewhere * Corregidor, an island in the Philippines also known as "The Rock" * Jamaica, an islan ...
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List Of Rock Formations In New Zealand
This is a list of rock formations in New Zealand based on their aesthetic and cultural importance. New Zealand's geomorphology is formed through an interaction between uplift, erosion and the underlying rock type. Most of the notable examples listed here are formed by selective erosion, for example waves and rivers can more easily erode sandstone than basalt and can also exploit joints or faults in the rock-mass. Some rocks like limestone (Waitomo Caves) and marble ( Takaka Hill) can also be dissolved in water which forms a distinctive karst geomorphology. Notable rock formations are also formed through constructive processes such as geothermal and volcanic deposits, and sedimentary deposition. North Island formations South Island formations Formations elsewhere Maps See also * List of caves of New Zealand * List of rock formations * Stratigraphy of New Zealand * Geomorphology Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") ...
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Norfolk Island
Norfolk Island (, ; Norfuk: ''Norf'k Ailen'') is an external territory of Australia located in the Pacific Ocean between New Zealand and New Caledonia, directly east of Australia's Evans Head and about from Lord Howe Island. Together with the neighbouring Phillip Island and Nepean Island, the three islands collectively form the Territory of Norfolk Island. At the 2021 census, it had inhabitants living on a total area of about . Its capital is Kingston. The first known settlers in Norfolk Island were East Polynesians but they had already departed when Great Britain settled it as part of its 1788 settlement of Australia. The island served as a convict penal settlement from 6 March 1788 until 5 May 1855, except for an 11-year hiatus between 15 February 1814 and 6 June 1825, when it lay abandoned. On 8 June 1856, permanent civilian residence on the island began when descendants of the ''Bounty'' mutineers were relocated from Pitcairn Island. In 1914 the UK handed Norfo ...
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Kerikeri
Kerikeri () is the largest town in Northland, New Zealand. It is a tourist destination north of Auckland and north of the northern region's largest city, Whangarei. It is sometimes called the Cradle of the Nation, as it was the site of the first permanent mission station in the country, and it has some of the most historic buildings in the country. A rapidly expanding centre of subtropical and allied horticulture, Kerikeri is in the Far North District of the North Island and lies at the western extremity of the Kerikeri Inlet, a northwestern arm of the Bay of Islands, where fresh water of the Kerikeri River enters the Pacific Ocean. The village was established by New Zealand's pioneering missionaries, who called it Gloucester Town, but the name did not endure. The Māori word ''Kerikeri'' was interpreted by said missionaries as Keddi Keddi or Kiddeekiddee, before the romanisation methods they used were revised to what is used today. In 1814, Samuel Marsden acquired lan ...
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Lake Manuwai
Lake Manuwai is a lake in the Northland Region of New Zealand. Located near Kerikeri in the Bay of Islands, it is part of the upper Waipapa stream. It is a reservoir created in the 1980's by the Ministry of Works along with Lake Waingaro to supply irrigation to Kerikeri's horticulture industry. In 1990, it was purchased by a cooperative of local horticulturalists and farmers under the name Kerikeri Irrigation Co Ltd. Uses An easement exists with the Far North District Council which allows public access for passive activities such as sailing, picnicking, swimming, kayaking, and fishing. The lake is stocked annually by Fish and Game with 400-500 rainbow trout fingerlings. Motorised craft are restricted on Lake Manuwai, though exceptions are made for safety, scientific, and maintenance use. See also *List of lakes in New Zealand This is a list of lakes in New Zealand. A lake's location is identified by the region and either the territorial authority or national ...
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Leigh, New Zealand
Leigh is a small coastal community in the north of the Auckland Region of New Zealand. It lies on the west side of Omaha Cove, a small inlet within Omaha Bay to the south of Cape Rodney. It is 13 km from Matakana, 21 km from Warkworth and approximately 92 km north of Auckland City. Leigh is the nearest town to Cape Rodney-Okakari Point Marine Reserve surrounding Te Hāwere-a-Maki / Goat Island. The reserve, the first of its type in New Zealand, is also the location for the University of Auckland's Marine Laboratory.Wises New Zealand Guide, 7th Edition, 1979. p.200. Demographics Statistics New Zealand describes Leigh as a rural settlement, which covers . Leigh is part of the larger Cape Rodney statistical area. Leigh had a population of 606 at the 2018 New Zealand census, an increase of 36 people (6.3%) since the 2013 census, and an increase of 105 people (21.0%) since the 2006 census. There were 261 households, comprising 306 males and 300 females, giving a se ...
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Waiheke Island
Waiheke Island (; Māori: ) is the second-largest island (after Great Barrier Island) in the Hauraki Gulf of New Zealand. Its ferry terminal in Matiatia Bay at the western end is from the central-city terminal in Auckland. It is the most populated island in the gulf, with permanent residents. Another estimated 3,400 have second homes or holiday homes on the island. It is New Zealand's most densely populated island, and the third most populated after the North and South Islands. It is the most accessible island in the gulf, with regular passenger and car-ferry services, a helicopter operator based on the island, and other air links. In November 2015, Lonely Planet rated Waiheke Island the fifth-best region in the world to visit in 2016. Geography Overview The island is off the coast of the North Island. It is in length from west to east, varies in width from , and has a surface area of . The coastline is , including of beaches. The port of Matiatia at the western end is ...
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Humic Substance
Humic substances (HS) are organic compounds that are important components of humus, the major organic fraction of soil, peat, and coal (and also a constituent of many upland streams, dystrophic lakes, and ocean water). For a long era in the 19th and 20th centuries, humic substances were often viewed through a lens of acid–base theory that described humic acids (HA), as organic acids, and their conjugate bases, humates, as important components of organic matter. Through this viewpoint humic acids were defined as organic substances extracted from soil that coagulate (form small solid pieces) when a strong-base extract is acidified, whereas fulvic acids (FA) are organic acids that remain soluble (stay dissolved) when a strong-base extract is acidified. The remaining alkali-insoluble part of humus would be termed humin. Humic matter in isolation is the result of a chemical extraction from the soil organic matter or the dissolved organic matter and represent the humic molecules dis ...
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Calcareous
Calcareous () is an adjective meaning "mostly or partly composed of calcium carbonate", in other words, containing lime or being chalky. The term is used in a wide variety of scientific disciplines. In zoology ''Calcareous'' is used as an adjectival term applied to anatomical structures which are made primarily of calcium carbonate, in animals such as gastropods, i.e., snails, specifically about such structures as the operculum, the clausilium, and the love dart. The term also applies to the calcium carbonate tests of often more or less microscopic Foraminifera. Not all tests are calcareous; diatoms and radiolaria have siliceous tests. The molluscs are calcareous, as are calcareous sponges ( Porifera), that have spicules which are made of calcium carbonate. In botany ''Calcareous grassland'' is a form of grassland characteristic of soils containing much calcium carbonate from underlying chalk or limestone rock. In medicine The term is used in pathology, for example i ...
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Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ...
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