|
Maruia Falls
The Maruia River is located in the northwestern South Island of New Zealand. It is a major tributary of the Buller River, flowing for 80 km before joining the larger river eight kilometres to the west of Murchison. The Maruia River rises in the Spenser Mountains, travelling first to the southwest before turning north for the last 50 km of its length. In its upper reaches, the river's valley forms the western approach to the Lewis Pass, the northernmost of the three main mountain passes across the Southern Alps. Hot springs are to be found close to the river in its upper reaches, and the spa of Maruia Springs is located five kilometres to the west of the Lewis Pass, 50 km southeast of Reefton. 3 km east of Springs Junction, the Maruia River flows through the deep and narrow Sluice Box gorge. The river cuts through a band of marble amongst the otherwise predominant greywacke. The Sluice Box, at the junction with the Alfred River, separates the upper and midd ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maruia River
The Maruia River is located in the northwestern South Island of New Zealand. It is a major tributary of the Buller River, flowing for 80 km before joining the larger river eight kilometres to the west of Murchison. The Maruia River rises in the Spenser Mountains, travelling first to the southwest before turning north for the last 50 km of its length. In its upper reaches, the river's valley forms the western approach to the Lewis Pass, the northernmost of the three main mountain passes across the Southern Alps. Hot springs are to be found close to the river in its upper reaches, and the spa of Maruia Springs is located five kilometres to the west of the Lewis Pass, 50 km southeast of Reefton. 3 km east of Springs Junction, the Maruia River flows through the deep and narrow Sluice Box gorge. The river cuts through a band of marble amongst the otherwise predominant greywacke. The Sluice Box, at the junction with the Alfred River, separates the upper and m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marble
Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or Dolomite (mineral), dolomite. Marble is typically not Foliation (geology), foliated (layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. Marble is commonly used for Marble sculpture, sculpture and as a building material. Etymology The word "marble" derives from the Ancient Greek (), from (), "crystalline rock, shining stone", perhaps from the verb (), "to flash, sparkle, gleam"; Robert S. P. Beekes, R. S. P. Beekes has suggested that a "Pre-Greek origin is probable". This Stem (linguistics), stem is also the ancestor of the English language, English word "marmoreal," meaning "marble-like." While the English term "marble" resembles the French language, French , most other European languages (with words like "marmoreal") more closely resemb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of The West Coast, New Zealand
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, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buller District
Buller District is one of 53 districts of New Zealand, and is within the West Coast Region. It covers Westport, Karamea, Reefton and Inangahua Junction. Buller District's overall land area is . The district is administered by the Buller District Council with the seat in Westport, in which 45% of the district's population live. History It is understood by the carbon dating of Umu (ovens) that the Maori people settled in this region some 700 years ago. The district takes its name from the Buller River, itself named for Charles Buller, a Member of Parliament in the United Kingdom of Great Britain and Ireland (UK) and director of the New Zealand Company, a UK-based company established in the early 19th century with a royal charter supporting colonisation efforts of New Zealand. During the period 1853 to 1876, the current area of Buller District was administered as part of Nelson Province. With the Abolition of Provinces Act 1876, much of the current area of Buller District w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1929 Murchison Earthquake
The 1929 Murchison earthquake occurred at 10:17 am on 17 June. It struck the Murchison region of the South Island, with an estimated magnitude of 7.3, and was felt throughout New Zealand. There were 17 deaths, mostly as a result of landslides triggered by the earthquake. The rumbling sound of the earthquake was loud enough to be heard at New Plymouth, more than 250 km (155 mi) away. Tectonic setting New Zealand sits astride the boundary between the Indo-Australian Plate and the Pacific Plate. In the South Island most of the displacement is taken up on the Alpine Fault passing to the north onto a set of strike-slip faults, the Marlborough Fault System. The sense of displacement across the plate boundary is oblique and most of the faults have a reverse component of slip. Some of the resulting deformation is accommodated within the plates themselves away from the boundary. The 1929 Murchison earthquake occurred on the White Creek Fault, located in the Buller Gorge. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maruia Falls 28
Maruia is a locality in the West Coast region of New Zealand. The Shenandoah Highway (State Highway 65) passes through it. Murchison is 65 km north, the Lewis Pass is 39 km to the south-east, and Reefton is 63 km west by road. The Maruia River flows past to the west. According to the 2013 New Zealand census The 2013 New Zealand census was the thirty-third national census. "The National Census Day" used for the census was on Tuesday, 5 March 2013. The population of New Zealand was counted as 4,242,048, – an increase of 214,101 or 5.3% over the 20 ..., Maruia and its surrounds have a population of 183, an increase of 9 people since the 2006 census. There were 96 males and 87 females. The principal activity is dairy farming. The community celebrated 100 years of settlement in the Maruia Valley in 2005. The Maruia Valley inspired the environmental lobby group, the Maruia Society (later changing its name to the Ecologic Foundation) and the Maruia Mail Order C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maruia Falls
The Maruia River is located in the northwestern South Island of New Zealand. It is a major tributary of the Buller River, flowing for 80 km before joining the larger river eight kilometres to the west of Murchison. The Maruia River rises in the Spenser Mountains, travelling first to the southwest before turning north for the last 50 km of its length. In its upper reaches, the river's valley forms the western approach to the Lewis Pass, the northernmost of the three main mountain passes across the Southern Alps. Hot springs are to be found close to the river in its upper reaches, and the spa of Maruia Springs is located five kilometres to the west of the Lewis Pass, 50 km southeast of Reefton. 3 km east of Springs Junction, the Maruia River flows through the deep and narrow Sluice Box gorge. The river cuts through a band of marble amongst the otherwise predominant greywacke. The Sluice Box, at the junction with the Alfred River, separates the upper and midd ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
:en:Department Of Conservation (New Zealand)
The Department of Conservation (DOC; Māori: ''Te Papa Atawhai'') is the public service department of New Zealand charged with the conservation of New Zealand's natural and historical heritage. An advisory body, the New Zealand Conservation Authority (NZCA) is provided to advise DOC and its ministers. In addition there are 15 conservation boards for different areas around the country that provide for interaction between DOC and the public. Function Overview The department was formed on 1 April 1987, as one of several reforms of the public service, when the ''Conservation Act 1987'' was passed to integrate some functions of the Department of Lands and Survey, the Forest Service and the Wildlife Service. This act also set out the majority of the department's responsibilities and roles. As a consequence of Conservation Act all Crown land in New Zealand designated for conservation and protection became managed by the Department of Conservation. This is about 30% of New Z ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greywacke
Greywacke or graywacke (German ''grauwacke'', signifying a grey, earthy rock) is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or lithic fragments set in a compact, clay-fine matrix. It is a texturally immature sedimentary rock generally found in Paleozoic strata. The larger grains can be sand- to gravel-sized, and matrix materials generally constitute more than 15% of the rock by volume. The term "greywacke" can be confusing, since it can refer to either the immature (rock fragment) aspect of the rock or its fine-grained (clay) component. The origin of greywacke was unknown until turbidity currents and turbidites were understood, since, according to the normal laws of sedimentation, gravel, sand and mud should not be laid down together. Geologists now attribute its formation to submarine avalanches or strong turbidity currents. These actions churn sediment and cause mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reefton, New Zealand
Reefton is a small town in the West Coast region of New Zealand, some 80 km northeast of Greymouth, in the Inangahua River valley. Ahaura is 44 km south-west of Reefton, Inangahua Junction is 34 km to the north, Maruia is 63 km to the east, and the Lewis Pass is 66 km to the south-east. In 1888, it was the first town in New Zealand and the Southern Hemisphere to be lit by electricity, generated by the Reefton Power Station. Reefton was a thriving gold mining town in the late 19th century, and gold mining lasted from the 1870s to the 1950s. Its economy is based on tourism, forestry, coal mining and farming. Reefton is home to the Inangahua County Library. Name The rich veins of gold found in a quartz reef near the town led to its name, originally spelled "Reef Town". Two nicknames in use soon after it was founded were "Rest Town" and "Quartzopolis". The main street, Broadway, was named after West Coast magistrate Charles Broad. The nearby Wealth of Na ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Island
The South Island, also officially named , is the larger of the two major islands of New Zealand in surface area, the other being the smaller but more populous North Island. It is bordered to the north by Cook Strait, to the west by the Tasman Sea, and to the south and east by the Pacific Ocean. The South Island covers , making it the world's 12th-largest island. At low altitude, it has an oceanic climate. The South Island is shaped by the Southern Alps which run along it from north to south. They include New Zealand's highest peak, Aoraki / Mount Cook at . The high Kaikōura Ranges lie to the northeast. The east side of the island is home to the Canterbury Plains while the West Coast is famous for its rough coastlines such as Fiordland, a very high proportion of native bush and national parks, and the Fox and Franz Josef Glaciers. The main centres are Christchurch and Dunedin. The economy relies on agriculture and fishing, tourism, and general manufacturing and services. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Alps (New Zealand)
The Southern Alps (; officially Southern Alps / Kā Tiritiri o te Moana) is a mountain range extending along much of the length of New Zealand's South Island, reaching its greatest elevations near the range's western side. The name "Southern Alps" generally refers to the entire range, although separate names are given to many of the smaller ranges that form part of it. The range includes the South Island's Main Divide, which separates the water catchments of the more heavily populated eastern side of the island from those on the west coast. Politically, the Main Divide forms the boundary between the Marlborough, Canterbury and Otago regions to the southeast and the Tasman and West Coast regions to the northwest. Names The Māori name of the range is , meaning "the Mirage of the Ocean". The English explorer James Cook bestowed the name ''Southern Alps'' on 23 March 1770, admiring their "prodigious height". p. 384. They had previously been noted by Abel Tasman in 1642, whose ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> 1929 Murchison Earthquake")
.svg "Click for more on -> South Island")
