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Mahurangi River
The Mahurangi River in northern New Zealand flows through the town of Warkworth and into Mahurangi Harbour, which opens into the outer Hauraki Gulf. The Left Branch of the river rises in the Dome and flows through the Dome Valley, while the Right Branch rises on Moir Hill. The lower part is a tidal estuary that ranges in depth from below approximately at the channel entrance to approximately further upstream. The Mahurangi Harbour provides a sheltered anchorage for private pleasure craft in all weathers. History Approximately 17,000 years ago during the Last Glacial Period when sea levels were significantly lower, the Mahurangi River flowed into the vast coastal plain that existed where the modern Hauraki Gulf exists. The river met the Waitematā Harbour (then a river) east of Kawau Island, and flowed north-east between modern day Little Barrier Island and Great Barrier Island, eventually emptying into the Pacific Ocean north of Great Barrier Island. In colonial New Zeala ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mahurangi Harbour
Mahurangi Harbour is a natural harbour in New Zealand. It is located on the north-eastern coast of the Auckland Region near the town of Warkworth, New Zealand, Warkworth, and empties into the Hauraki Gulf. Geography The Mahurangi Harbour is a drowned river valley. Approximately 17,000 years ago during the Last Glacial Period when sea levels were significantly lower, the freshwater Mahurangi River flowed into the vast coastal plain that existed where the modern Hauraki Gulf exists. The river met the Waitematā Harbour (then a river) east of Kawau Island, and flowed north-east between modern day Little Barrier Island and Great Barrier Island, eventually emptying into the Pacific Ocean north of Great Barrier Island. The modern harbour formed approximately 7,200 years ago at the end of the last glacial maximum, when the forested valley was flooded by rising sea levels. Land use within the harbour's catchment basin has been changing, and models predict an increase in sedimentat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Institute Of Water And Atmospheric Research
The National Institute of Water and Atmospheric Research or NIWA ( mi, Taihoro Nukurangi), is a Crown Research Institute of New Zealand. Established in 1992, NIWA conducts research across a broad range of disciplines in the environmental sciences. It also maintains nationally and, in some cases, internationally important environmental monitoring networks, databases, and collections. , NIWA had 697 staff spread across 14 sites in New Zealand and one in Perth, Australia. Its head office is in Auckland, with regional offices in Hamilton, Wellington, Christchurch, Nelson, and Lauder (Central Otago). It also has small field teams, focused mostly on hydrology, stationed in Bream Bay, Lake Tekapo, Rotorua, Napier, Whanganui, Greymouth, Alexandra, and Dunedin. NIWA maintains a fleet of about 30 vessels for freshwater, marine, and atmospheric research. Mission statement "NIWA's mission is to conduct leading environmental science to enable the sustainable management of natural re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of The Auckland Region
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland Libraries
Auckland Libraries is the public library system for the Auckland Region of New Zealand. It was created when the seven separate councils in the Auckland region merged in 2010. It is currently the largest public-library network in the Southern Hemisphere with 55 branches from Wellsford to Waiuku. Currently from March 2021, the region has a total of 56 branches. History In November 2010, Auckland's local councils merged to create the Auckland Council. As a result of this process, the seven public library systems within the region were combined to form Auckland Libraries. The following library networks were amalgamated, forming Auckland Libraries: * Auckland City Libraries * Bookinopolis (in the Franklin District) * Manukau Libraries * North Shore Libraries * Papakura Library ServicesThe Sir Edmund Hillary Library * Rodney Libraries * Waitakere Libraries The process of amalgamation In the years leading up to the merger of the library systems within Auckland, the separate library ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Footbridge
A footbridge (also a pedestrian bridge, pedestrian overpass, or pedestrian overcrossing) is a bridge designed solely for pedestrians.''Oxford English Dictionary'' While the primary meaning for a bridge is a structure which links "two points at a height above the ground", a footbridge can also be a lower structure, such as a boardwalk, that enables pedestrians to cross wet, fragile, or marshy land. Bridges range from stepping stones–possibly the earliest man-made structure to "bridge" water–to elaborate steel structures. Another early bridge would have been simply a fallen tree. In some cases a footbridge can be both functional and artistic. For rural communities in the developing world, a footbridge may be a community's only access to medical clinics, schools, businesses and markets. Simple suspension bridge designs have been developed to be sustainable and easily constructed in such areas using only local materials and labor. An enclosed footbridge between two buildings ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tramway Track
Tramway track is used on tramways or light rail operations. Grooved rails (or girder rails) are often used to provide a protective flangeway in the trackwork in city streets. Like standard rail tracks, tram tracks consist of two parallel steel rails. Tram rails can be placed on several surfaces, such as with standard rails on sleepers like railway tracks, or with grooved rails on concrete sleepers into street surfaces ( pavement) for street running. Tram rails in street have the disadvantage that they pose a risk to cyclists. An alternative is to lay tracks into non-road grass turf surfaces; this is known as ''grassed track'' (or ''track in a lawn''), introduced in Liverpool in 1924 - although grassed track is common in rural tramways. History Tramway tracks have been in existence since the mid-16th century. They were previously made of wood, but during the late 18th century iron and later steel came into use prominently. The first street tramways were laid in 1832 in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1877 Iquique Earthquake
The 1877 Iquique earthquake occurred at 21:16 local time on 9 May (0:59 on 10 May UTC). It had a magnitude of 8.5 on the surface wave magnitude scale. Other estimates of its magnitude have been as high as 8.9 and 9.0 (based on the size of the tsunami). It had a maximum intensity of XI (Extreme) on the Mercalli intensity scale and triggered a devastating tsunami. A total of 2,385 people died, mainly in Fiji. Historical context Affected areas in what was then part of Bolivia, but is now the Antofagasta region of Chile, had during this period been subject to the Atacama border dispute between the two countries. Under the 1874 boundary treaty between Bolivia and Chile, the border between the two nations as of 1877 followed the 24th parallel south. The terms of that treaty required that Bolivia not levy taxes on Chilean companies mining nitrates between the 23rd and 24th parallels (including the city of Antofagasta) for 25 years, except for agreed duties to be shared between t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ballast
Ballast is material that is used to provide stability to a vehicle or structure. Ballast, other than cargo, may be placed in a vehicle, often a ship or the gondola of a balloon or airship, to provide stability. A compartment within a boat, ship, submarine, or other floating structure that holds water is called a ballast tank. Water should move in and out from the ballast tank to balance the ship. In a vessel that travels on the water, the ballast will remain below the water level, to counteract the effects of weight above the water level. The ballast may be redistributed in the vessel or disposed of altogether to change its effects on the movement of the vessel. History The basic concept behind the ballast tank can be seen in many forms of aquatic life, such as the blowfish or members of the argonaut group of octopus. The concept has been invented and reinvented many times by humans to serve a variety of purposes. In the fifteenth and sixteenth century, the ballast "did not c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Agathis Australis
''Agathis australis'', commonly known by its Māori name kauri (), is a coniferous tree in the family '' Araucariaceae'', found north of 38°S in the northern regions of New Zealand's North Island. It is the largest (by volume) but not tallest species of tree in New Zealand, standing up to 50 m tall in the emergent layer above the forest's main canopy. The tree has smooth bark and small narrow leaves. Other common names to distinguish ''A. australis'' from other members of ''Agathis'' are southern kauri and New Zealand kauri. With its novel soil interaction and regeneration pattern it can compete with faster growing angiosperms. Because it is such a conspicuous species, forest containing kauri is generally known as kauri forest, although kauri need not be the most abundant tree. In the warmer northern climate, kauri forests have a higher species richness than those found further south. Kauri even act as a foundation species that modify the soil under their canopy to cre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Portland Cement
Portland cement is the most common type of cement in general use around the world as a basic ingredient of concrete, mortar, stucco, and non-specialty grout. It was developed from other types of hydraulic lime in England in the early 19th century by Joseph Aspdin, and is usually made from limestone. It is a fine powder, produced by heating limestone and clay minerals in a kiln to form clinker, grinding the clinker, and adding 2 to 3 percent of gypsum. Several types of portland cement are available. The most common, called ordinary portland cement (OPC), is grey, but white Portland cement is also available. Its name is derived from its resemblance to Portland stone which was quarried on the Isle of Portland in Dorset, England. It was named by Joseph Aspdin who obtained a patent for it in 1824. His son William Aspdin is regarded as the inventor of "modern" portland cement due to his developments in the 1840s. The low cost and widespread availability of the limesto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colonial New Zealand
The Colony of New Zealand was a Crown colony of the United Kingdom of Great Britain and Ireland that encompassed the islands of New Zealand from 1841 to 1907. The power of the British government was vested in the Governor of New Zealand, as the representative of their monarch. The colony had three capitals: Old Russell in 1841; Auckland from 1841 to 1865; and Wellington, which was the capital until the colony's reorganisation into a Dominion, and continues to be the capital of New Zealand till the present day. In 1852, the colony was granted self-government with the passage of the New Zealand Constitution Act 1852. Subsequently, the first parliament was elected in 1853, and responsible government was established in 1856. In 1907, the colony became the Dominion of New Zealand, which heralded a more explicit recognition of self-government within the British Empire. History Establishment Following a proclamation of sovereignty over New Zealand from Sydney in January ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
