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List Of Rock Formations Of 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 Geology of New Zealand, 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 Joint (geology), joints or Fault (geology), 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 References {{DEFAULTSOR ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geomorphology
Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field. Overview Earth's surface is modified by a combination of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the coastal geography. Surface processes co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dome Of Saint Paul
A dome () is an architectural element similar to the hollow upper half of a sphere. There is significant overlap with the term cupola, which may also refer to a dome or a structure on top of a dome. The precise definition of a dome has been a matter of controversy and there are a wide variety of forms and specialized terms to describe them. A dome can rest directly upon a rotunda wall, a drum, or a system of squinches or pendentives used to accommodate the transition in shape from a rectangular or square space to the round or polygonal base of the dome. The dome's apex may be closed or may be open in the form of an oculus, which may itself be covered with a roof lantern and cupola. Domes have a long architectural lineage that extends back into prehistory. Domes were built in ancient Mesopotamia, and they have been found in Persian, Hellenistic, Roman, and Chinese architecture in the ancient world, as well as among a number of indigenous building traditions throughout the world ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mangapohue Natural Bridge
The Mangapohue Natural Bridge consists of two rock arches formed by the Mangapohue Stream in the Marokopa River valley near Waitomo, New Zealand. The 17 m high limestone arches are a remnant of an ancient cave system. The smaller lower rock arch spans the Mangapohue Stream and cannot be walked through, while the larger upper arch is situated straight above the lower arch and contains a platform to view the stalactites on the upper arch's ceiling. The arches can be reached by the sealed Te Anga Road from State Highway 3 approximately 25 km west of the Waitomo Caves. From the carpark, the wheelchair-friendly walk takes 5 minutes to reach the natural bridge. The walk leads through a scenic limestone gorge, crossing the stream once on a timber bridge, and ending at a viewing platform below the rock arches. Steps lead to a further viewing platform between the lower and upper arch. A track also continues some 15 minutes further over farmland. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bottom Rock Arch Of Mangapohue Natural Bridge Over Mangapohue Stream
Bottom may refer to: Anatomy and sex * Bottom (BDSM), the partner in a BDSM who takes the passive, receiving, or obedient role, to that of the top or dominant * Bottom (sex), a term used by gay couples and BDSM * Buttocks or bottom, part of the anatomy on the posterior of the pelvic region of apes and humans, and many other bipeds or quadrupeds Arts, entertainment, and media * ''Bottom'' (TV series), a British sitcom and stage show * "Bottom", a song by Puddle of Mudd from '' Life On Display'' * "Bottom", a song by Tool from '' Undertow'' * Nick Bottom, a character from Shakespeare's ''A Midsummer Night's Dream'' * ''The Bottoms'' (novel), a 2000 novel by Joe R. Lansdale * ''Bottoms'', a 1966 film by Yoko Ono Geography * Bottom (valley), the floor of a valley ** List of geographical bottoms, list of geographical features called "bottom" * Bottomland (freshwater ecology), low-lying alluvial land adjacent to a river *Foggy Bottom, a neighborhood in Washington, D.C. * Lowe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lion Rock (New Zealand)
Lion Rock is a rocky headland located on Piha Beach in the Waitākere Ranges area of the Auckland Region, New Zealand. Geography The rock is located to the south of Piha beach, close to the major settlement at Piha. The Piha Stream flows into the Tasman Sea directly south of the rock. Geology The island is a volcanic plug of the Miocene era Waitākere Volcano, composed of stratified rudite and intrusive andesite. The rock is what remains of one of the volcano's funnel-shaped vents on the eastern side of the mountain, which was uplifted from the sea 17 million years ago. As the volcano aged and eroded, the Lion Rock vent filled with collapsed lava, scoria and volcanic bombs, until it formed into its modern-day shape. History The traditional name for the rock is Te Piha, and is a name that was applied to the wider area. The name Te Piha came from the pattern made when waves hit against the rock. Lion Rock is in the rohe of Te Kawerau ā Maki, and was the location of islan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lion Rock, Piha
The lion (''Panthera leo'') is a large cat of the genus ''Panthera'' native to Africa and India. It has a muscular, broad-chested body; short, rounded head; round ears; and a hairy tuft at the end of its tail. It is sexually dimorphic; adult male lions are larger than females and have a prominent mane. It is a social species, forming groups called ''prides''. A lion's pride consists of a few adult males, related females, and cubs. Groups of female lions usually hunt together, preying mostly on large ungulates. The lion is an apex and keystone predator; although some lions scavenge when opportunities occur and have been known to hunt humans, lions typically don't actively seek out and prey on humans. The lion inhabits grasslands, savannas and shrublands. It is usually more diurnal than other wild cats, but when persecuted, it adapts to being active at night and at twilight. During the Neolithic period, the lion ranged throughout Africa and Eurasia from Southeast Europe to In ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Koutu Boulders
Koutu is a suburb of Rotorua in the Bay of Plenty Region of New Zealand's North Island. Koutu was originally a home for the people of Ngati Whakaue and Ngāti Uenukukopako and has been in existence since before the establishment of Rotorua Township. It is located on the southwest shore of Lake Rotorua. The suburb has one marae. Koutu or Karenga Marae and Tumahaurangi meeting house is a meeting place of the Ngāti Whakaue hapū of Ngāti Karenga. Transport Koutu sits on State Highway 5 (New Zealand), State Highway 5. Koutu received a railway in 1894 when the Rotorua Branch line opened. It operated for over a century. In 1989, the last 2.4 km into central Rotorua closed, and a goods yard near industries in Koutu became the end of the line. Passenger trains from Auckland had ceased operating in 1968, but, ironically, a new service began two years after the railway was cut back to Koutu. Called the ''Geyserland Express'', it first operated on 9 December 1991 and terminated at a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Koutu Boulder4
Koutu is a suburb of Rotorua in the Bay of Plenty Region of New Zealand's North Island. Koutu was originally a home for the people of Ngati Whakaue and Ngāti Uenukukopako and has been in existence since before the establishment of Rotorua Township. It is located on the southwest shore of Lake Rotorua. The suburb has one marae. Koutu or Karenga Marae and Tumahaurangi meeting house is a meeting place of the Ngāti Whakaue hapū of Ngāti Karenga. Transport Koutu sits on State Highway 5. Koutu received a railway in 1894 when the Rotorua Branch line opened. It operated for over a century. In 1989, the last 2.4 km into central Rotorua closed, and a goods yard near industries in Koutu became the end of the line. Passenger trains from Auckland had ceased operating in 1968, but, ironically, a new service began two years after the railway was cut back to Koutu. Called the ''Geyserland Express'', it first operated on 9 December 1991 and terminated at a small platform north of Lak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kupe's Sail
Kupe's Sail ( mi, Ngā Rā-a-Kupe) is a geological formation near the eastern end of Palliser Bay at the southern end of the North Island of New Zealand. It is composed of sedimentary rock which has been thrust up in an earthquake, resulting in a characteristic flat triangular ridge having the appearance of the kind of sail regularly used by Pacific explorers such as Kupe Kupe ( ~1180-1320) was a legendary Polynesian explorer, navigator and great rangatira of Hawaiki, who is said to have been the first human to discover New Zealand. Whether Kupe existed historically is likely but difficult to confirm. He is g .... References1966 Encyclopedia of New Zealand [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Horeke Basalts
The Horeke basalts is a disused formation that contained Miocene-Pliocene basalt lava flows that covered a large area in central Northland Region of New Zealand, and in places forms a high plateau around Okaihau. Wairere Boulders is a nature park providing walkways through boulders of basalt, derived by erosion of one of these older basalt flows that used to be included in the Horeke Basalt and are now included in the Kerikeri Volcanic Group. Origin The boulders in the Wairere valley are the erosional remnants of a lava flow out of a volcano near Lake Ōmāpere (near Kaikohe) that has been dated as approximately 2.8 million years old. There are two dates for these Horeke basalts: one at 2.84 and the other at 2.67 million years. There is a slight difference in chemistry in the two rocks that have been dated suggesting that the eruption took the form of several flows that once blanketed the high ground to the east of Horeke. Formation Erosion of the clay underlay ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
