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Omarama Clay Cliffs
The Omarama Clay Cliffs, also known as the Ahuriri River Clay Cliffs and the Clay Cliffs Paritea are a group of cliffs in southern New Zealand. They are located close to the north bank of the Ahuriri River, some 10 km to the west of the township of Omarama. The cliffs serve as a tourist attraction in the area and they are privately owned. There is a fee to park. Formation The cliffs are made up of layers of silt and gravel that were formed during glacial erosion around two million years ago, and are part of the Hawkdun Group of sediments. The cliffs were uplifted by the nearby Ostler Fault Ostler is a surname, and may refer to: People *Andreas Ostler (1921–1988), German Olympic bobsledder *Blake Ostler (born 1955), American attorney *Dominic Ostler (born 1970), English cricketer * Nicholas Ostler (born 1952), British linguist *Will .... References Tourist attractions in New Zealand Cliffs of Oceania Waitaki District Rock formations of Canterbury, New Zealand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Omarama Clay Cliffs
The Omarama Clay Cliffs, also known as the Ahuriri River Clay Cliffs and the Clay Cliffs Paritea are a group of cliffs in southern New Zealand. They are located close to the north bank of the Ahuriri River, some 10 km to the west of the township of Omarama. The cliffs serve as a tourist attraction in the area and they are privately owned. There is a fee to park. Formation The cliffs are made up of layers of silt and gravel that were formed during glacial erosion around two million years ago, and are part of the Hawkdun Group of sediments. The cliffs were uplifted by the nearby Ostler Fault Ostler is a surname, and may refer to: People *Andreas Ostler (1921–1988), German Olympic bobsledder *Blake Ostler (born 1955), American attorney *Dominic Ostler (born 1970), English cricketer * Nicholas Ostler (born 1952), British linguist *Will .... References Tourist attractions in New Zealand Cliffs of Oceania Waitaki District Rock formations of Canterbury, New Zealand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also fea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ahuriri River
The Ahuriri River is a river in the Canterbury and Otago Regions of the South Island of New Zealand. The headwaters are on the eastern flanks of the Southern Alps. The river flows for through the southernmost part of the Mackenzie Basin before reaching the Ahuriri Arm of Lake Benmore, one of the lakes in the Waitaki hydroelectric project. From there, the waters join with those of the Waitaki, which has its outflow in the Pacific Ocean. Much of the upper portion of the river is in the Ahuriri Conservation Park, and it is a well-regarded fly fishing river, supporting both brown and rainbow trout. A notable rock formation, the Omarama or Ahuriri River Clay Cliffs, is located close to the river's north bank some 10 kilometres west of the township of Omarama Omarama is a small town (population 291 at 2018 census) at the junction of State Highways 8 and 83, near the southern end of the Mackenzie Basin, in the South Island of New Zealand. Omarama is in the Waitaki Di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Omarama
Omarama is a small town (population 291 at 2018 census) at the junction of State Highways 8 and 83, near the southern end of the Mackenzie Basin, in the South Island of New Zealand. Omarama is in the Waitaki District, in the southern Canterbury region. The Ahuriri River is a short distance to the north of the township. Omarama is 30 km (20 minutes drive) southwest of Twizel, 40 km (30 minutes drive) southeast of Lake Ōhau and 32 km (21 minutes drive) northeast of the Lindis Pass. Omarama is primarily a rural service centre, providing local farmers and other residents with necessities and facilities such as grocery shopping, fuel and mechanical services, as well as a post shop. In more recent years these and similar services have expanded moderately, due to the increase in new residents and visitors, including anglers, artists, astronomers, sailplane enthusiasts, skiers and general tourists. A significant proportion of permanent village residents are employee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tourist Attraction
A tourist attraction is a place of interest that tourists visit, typically for its inherent or an exhibited natural or cultural value, historical significance, natural or built beauty, offering leisure and amusement. Types Places of natural beauty such as beaches, tropical island resorts, national parks, mountains, deserts and forests, are examples of traditional tourist attractions which people may visit. Cultural tourist attractions can include historical places, sites of significant historic event, monuments, ancient temples, zoos, aquaria, museums and art galleries, botanical gardens, buildings and structures (such as forts, castles, libraries, former prisons, skyscrapers, bridges), theme parks and carnivals, living history museums, public art (sculptures, statues, murals), ethnic enclave communities, historic trains and cultural events. Factory tours, industrial heritage, creative art and crafts workshops are the object of cultural niches like industrial tourism and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silt
Silt is granular material of a size between sand and clay and composed mostly of broken grains of quartz. Silt may occur as a soil (often mixed with sand or clay) or as sediment mixed in suspension with water. Silt usually has a floury feel when dry, and lacks plasticity when wet. Silt also can be felt by the tongue as granular when placed on the front teeth (even when mixed with clay particles). Silt is a common material, making up 45% of average modern mud. It is found in many river deltas and as wind-deposited accumulations, particularly in central Asia, north China, and North America. It is produced in both very hot climates (through such processes as collisions of quartz grains in dust storms) and very cold climates (through such processes as glacial grinding of quartz grains.) Loess is soil rich in silt which makes up some of the most fertile agricultural land on Earth. However, silt is very vulnerable to erosion, and it has poor mechanical properties, making construction ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratigraphy Of New Zealand
This 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. Names for particular rock units have two parts, a proper name which is almost always a geographic location where the rock is found and a hierarchical rank (e.g. Waitematā Group). This ranking system starts with individual 'beds' of rock which can be grouped into 'members', members are grouped into 'formations', formations into 'subgroups' then 'groups'. In New Zealand, groups are further combined into 'supergroups' or for basement rocks into terranes. Not all of these hierarchical layers are necessarily present within a part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ostler Fault or ostler, a stableman
{{disambiguation, surname ...
Ostler is a surname, and may refer to: People * Andreas Ostler (1921–1988), German Olympic bobsledder *Blake Ostler (born 1955), American attorney *Dominic Ostler (born 1970), English cricketer *Nicholas Ostler (born 1952), British linguist *William Ostler (died 1614), English actor *Rob Ostlere, English actor * Gordon Ostlere (1921–2017), English surgeon and anaesthetist Other uses * Hostler A hostler or ostler is a groom or stableman, who is employed in a stable to take care of horses, usually at an inn. In the twentieth century the word came to be used in railroad industry for a type of train driver. Etymology The word is spelled ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tourist Attractions In New Zealand
Tourism is travel for pleasure or business; also the theory and practice of touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tours. The World Tourism Organization defines tourism more generally, in terms which go "beyond the common perception of tourism as being limited to holiday activity only", as people "travelling to and staying in places outside their usual environment for not more than one consecutive year for leisure and not less than 24 hours, business and other purposes". Tourism can be domestic (within the traveller's own country) or international, and international tourism has both incoming and outgoing implications on a country's balance of payments. Tourism numbers declined as a result of a strong economic slowdown (the late-2000s recession) between the second half of 2008 and the end of 2009, and in consequence of the outbreak of the 2009 H1N1 influenza virus, but slowly recovered until the COVID-19 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
