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Shag Point
Shag Point / Matakaea is a headland and township in East Otago, New Zealand. It is located close to State Highway 1 nine kilometres to the northeast of Palmerston, at the southern end of a long open bay known as Katiki Beach. The point itself is a hilly promontory between Katiki Beach and the mouth of the Shag River. Both the river and point take their English name from the shag, a species of cormorant. A historic Māori site, the Matakaea/Shag Point Occupation Site, is located close to the headland. It is listed as a Category II site by Heritage New Zealand. Geologically, the area is an exemplar of the Katiki Formation, and the site of the discovery of the plesiosaur ''Kaiwhekea katiki ''Kaiwhekea'' () is an extinct genus of plesiosaur from the Late Cretaceous (Maastrichtian age) of what is now New Zealand. History of discovery The type species, ''Kaiwhekea katiki'', was first described by Arthur Cruickshank and Ewan Fordyc ...''. References Headlands of Ota ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shag Point
Shag Point / Matakaea is a headland and township in East Otago, New Zealand. It is located close to State Highway 1 nine kilometres to the northeast of Palmerston, at the southern end of a long open bay known as Katiki Beach. The point itself is a hilly promontory between Katiki Beach and the mouth of the Shag River. Both the river and point take their English name from the shag, a species of cormorant. A historic Māori site, the Matakaea/Shag Point Occupation Site, is located close to the headland. It is listed as a Category II site by Heritage New Zealand. Geologically, the area is an exemplar of the Katiki Formation, and the site of the discovery of the plesiosaur ''Kaiwhekea katiki ''Kaiwhekea'' () is an extinct genus of plesiosaur from the Late Cretaceous (Maastrichtian age) of what is now New Zealand. History of discovery The type species, ''Kaiwhekea katiki'', was first described by Arthur Cruickshank and Ewan Fordyc ...''. References Headlands of Ota ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Otago
East Otago is the name given to that part of Otago, in the South Island of New Zealand that lies directly to the north of Dunedin. To the south, its limit is approximately the rough hill pass of the Kilmog, 25 kilometres north of Dunedin city centre, and in the north the limit is the Shag River. The population of East Otago is 2,500 (est 2001) Expected population in 2006 is 3,000 with 1,400 expecting to live in the Main town of Waikouaiti Census provisional count for East Otago as of 2006 was 4,991 Census provisional count for East Otago towns was: *Waikouaiti: 1,620 *Palmerston: 1,246 *Karitane: 720 *Dunback: 320 *Moeraki: 682 4,588 Live in the 5 main centers 403 Live in the rural areas Total: 4,991 The area contains two main towns, Waikouaiti and Palmerston along with the smaller settlements of Karitane and Dunback. The name East Otago has fallen somewhat out of favour since the expansion of the city limits of Dunedin to encompass much of this area in the 1990s. See ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand State Highway 1
State Highway 1 (SH 1) is the longest and most significant road in the New Zealand road network, running the length of both main islands. It appears on road maps as SH 1 and on road signs as a white number 1 on a red shield, but it has the official designations SH 1N in the North Island, SH 1S in the South Island. SH 1 is long, in the North Island and in the South Island. Since 2010 new roads have reduced the length from . For the majority of its length it is a two-lane single carriageway, with at-grade intersections and property accesses, in both rural and urban areas. These sections have some passing lanes. Around of SH 1 is of motorway or expressway standard : in the North Island and in the South Island. Route North Island (SH 1N) SH 1 starts at Cape Reinga, at the northwestern tip of the Aupouri Peninsula, and since April 2010 has been sealed (mainly with either chipseal or asphalt) for its entire length. From Waitiki Landing south of Cape Reinga, SH 1 trav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palmerston, New Zealand
The town of Palmerston, in New Zealand's South Island, lies 50 kilometres to the north of the city of Dunedin. It is the largest town in the Waihemo Ward of the Waitaki District, with a population of 890 residents. Palmerston grew at a major road junction: State Highway 1 links Dunedin and Waikouaiti to the south with Oamaru and Christchurch to the north, while State Highway 85 (known colloquially as "The Pigroot") heads inland to become the principal highway of the Maniototo. The Main South Line railway passes through the town and the Seasider tourist train travels from Dunedin to Palmerston and back once or twice a week. From 1880 until 1989, the town acted as the junction between the main line and a branch line that ran inland, the Dunback and Makareao Branches. Palmerston stands near the banks of the Shag River, five kilometres inland from the Pacific coast. Between it and the sea stands the lone hill of Puketapu (Māori for ''sacred hill'', known by Southerners as Holy Hil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shag River (Otago)
The Waihemo / Shag River is located in Otago in the South Island of New Zealand. It rises in the Kakanui Range, flowing southeast for , or before reaching the Pacific Ocean on the south side of Shag Point / Matakaea, east of Palmerston. The Dunback Branch railway that operated from the 1880s to 1989 largely followed the route of the river from its junction with the Main South Line near Shag Point township to its terminus in Dunback. The small- to medium-sized river has been adversely affected over the past decades by farming practices in the area. Much of its length is overgrown with willow Willows, also called sallows and osiers, from the genus ''Salix'', comprise around 400 speciesMabberley, D.J. 1997. The Plant Book, Cambridge University Press #2: Cambridge. of typically deciduous trees and shrubs, found primarily on moist so ...s, and during the summer its flow can become significantly reduced. In 1985, the name of the river was gazetted as Shag River (Waihemo). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cormorant
Phalacrocoracidae is a family of approximately 40 species of aquatic birds commonly known as cormorants and shags. Several different classifications of the family have been proposed, but in 2021 the IOC adopted a consensus taxonomy of seven genera. The great cormorant (''Phalacrocorax carbo'') and the common shag (''Gulosus aristotelis'') are the only two species of the family commonly encountered in Britain and Ireland and "cormorant" and "shag" appellations have been later assigned to different species in the family somewhat haphazardly. Cormorants and shags are medium-to-large birds, with body weight in the range of and wing span of . The majority of species have dark feathers. The bill is long, thin and hooked. Their feet have webbing between all four toes. All species are fish-eaters, catching the prey by diving from the surface. They are excellent divers, and under water they propel themselves with their feet with help from their wings; some cormorant species have been ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori People
The Māori (, ) are the indigenous Polynesian people of mainland New Zealand (). Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed their own distinctive culture, whose language, mythology, crafts, and performing arts evolved independently from those of other eastern Polynesian cultures. Some early Māori moved to the Chatham Islands, where their descendants became New Zealand's other indigenous Polynesian ethnic group, the Moriori. Initial contact between Māori and Europeans, starting in the 18th century, ranged from beneficial trade to lethal violence; Māori actively adopted many technologies from the newcomers. With the signing of the Treaty of Waitangi in 1840, the two cultures coexisted for a generation. Rising tensions over disputed land sales led to conflict in the 1860s, and massive land confiscations, to which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
NZHPT
Heritage New Zealand Pouhere Taonga (initially the National Historic Places Trust and then, from 1963 to 2014, the New Zealand Historic Places Trust) ( mi, Pouhere Taonga) is a Crown entity with a membership of around 20,000 people that advocates for the protection of ancestral sites and heritage buildings in New Zealand. It was set up through the Historic Places Act 1954 with a mission to "...promote the identification, protection, preservation and conservation of the historical and cultural heritage of New Zealand" and is an autonomous Crown entity. Its current enabling legislation is the Heritage New Zealand Pouhere Taonga Act 2014. History Charles Bathurst, 1st Viscount Bledisloe gifted the site where the Treaty of Waitangi was signed to the nation in 1932. The subsequent administration through the Waitangi Trust is sometimes seen as the beginning of formal heritage protection in New Zealand. Public discussion about heritage protection occurred in 1940 in conjunction with th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heritage New Zealand
Heritage New Zealand Pouhere Taonga (initially the National Historic Places Trust and then, from 1963 to 2014, the New Zealand Historic Places Trust) ( mi, Pouhere Taonga) is a Crown entity with a membership of around 20,000 people that advocates for the protection of ancestral sites and heritage buildings in New Zealand. It was set up through the Historic Places Act 1954 with a mission to "...promote the identification, protection, preservation and conservation of the historical and cultural heritage of New Zealand" and is an autonomous Crown entity. Its current enabling legislation is the Heritage New Zealand Pouhere Taonga Act 2014. History Charles Bathurst, 1st Viscount Bledisloe gifted the site where the Treaty of Waitangi was signed to the nation in 1932. The subsequent administration through the Waitangi Trust is sometimes seen as the beginning of formal heritage protection in New Zealand. Public discussion about heritage protection occurred in 1940 in conjunction with t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Katiki Formation
The Katiki Formation is a Late Cretaceous (Campanian to Maastrichtian, or Haumurian in the regional stratigraphy) geologic formation of the South Island of New Zealand.Katiki Formation in the remains of '''', named after the formation, are among the |
Kaiwhekea Katiki
''Kaiwhekea'' () is an extinct genus of plesiosaur from the Late Cretaceous (Maastrichtian age) of what is now New Zealand. History of discovery The type species, ''Kaiwhekea katiki'', was first described by Arthur Cruickshank and Ewan Fordyce in 2002. ''Kaiwhekea'' was approximately long and weighed in body mass. It lived around the middle Maastrichtian. The single known specimen, found in the Katiki Formation near Shag Point on the coast of Otago, is nearly complete, and is on display at the Otago Museum in Dunedin, New Zealand. Classification ''Kaiwhekea'' has been placed as an aristonectine plesiosaur close to ''Aristonectes'' (O'Keefe and Street, 2009). In 2010, ''Kaiwhekea'' was transferred to Leptocleididae, but more recent analyses do not find the same result. The following cladogram shows the placement of ''Kaiwhekea'' within Elasmosauridae following an analysis by Rodrigo A. Otero, 2016: See also * List of plesiosaur genera * Timeline of plesiosaur research ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
