scholarly journals Sequent Economies in Kuku: A Study of a Rural Locality in New Zealand

2021 ◽  
Author(s):  
◽  
John Rodford Wehipeihana
Keyword(s):  
New Zealand ◽  
Coastal Plain ◽  
Capital City ◽  
The West ◽  
Railway Line ◽  
The North ◽  
State Highway ◽  
Tasman Sea ◽  
Rural Locality

<p>Today, the majority of travellers journeying in the North Island of New Zealand, from Wellington to points north, e.g. Palmerston North or Wanganui, travel the length of the Horowhenua coastal plain, which sole routeway is bordered by the Tararua foothills to the east and by the Tasman Sea to the west. At a point some 52 miles north of the capital city and approximately 4 miles south of Levin, the motorist passes over a white bridge near which stands a dairy factory, and at a distance, a Maori meeting house. At the end of the mile-long stretch of State highway, an elevated by-pass affords a view of fenced paddocks, closely-cultivated fields, a railway line and a river. (See frontispiece.) As such scenes are common on many lowland pockets of the North Island of New Zealand, they mean little to the average traveller who crosses the Ohau River and pursues his northward course.</p>

scholarly journals Sequent Economies in Kuku: A Study of a Rural Locality in New Zealand

2021 ◽  
Author(s):  
◽  
John Rodford Wehipeihana
Keyword(s):  
New Zealand ◽  
Coastal Plain ◽  
Capital City ◽  
The West ◽  
Railway Line ◽  
The North ◽  
State Highway ◽  
Tasman Sea ◽  
Rural Locality

<p>Today, the majority of travellers journeying in the North Island of New Zealand, from Wellington to points north, e.g. Palmerston North or Wanganui, travel the length of the Horowhenua coastal plain, which sole routeway is bordered by the Tararua foothills to the east and by the Tasman Sea to the west. At a point some 52 miles north of the capital city and approximately 4 miles south of Levin, the motorist passes over a white bridge near which stands a dairy factory, and at a distance, a Maori meeting house. At the end of the mile-long stretch of State highway, an elevated by-pass affords a view of fenced paddocks, closely-cultivated fields, a railway line and a river. (See frontispiece.) As such scenes are common on many lowland pockets of the North Island of New Zealand, they mean little to the average traveller who crosses the Ohau River and pursues his northward course.</p>

Provenance of titanomagnetite in ironsands on the west coast of the North Island, New Zealand

2017 ◽  
Vol 178 ◽  
pp. 23-34 ◽  
Author(s):  
R.L. Brathwaite ◽  
M.F. Gazley ◽  
A.B. Christie
Keyword(s):  
New Zealand ◽  
West Coast ◽  
The West ◽  
The North

Invasion of the New Zealand Coastline by European Sea-Rocket (Cakile maritima) and American Sea-Rocket (Cakile edentula)

2011 ◽  
Vol 4 (2) ◽  
pp. 260-263 ◽  
Author(s):  
Roger D. Cousens ◽  
Jane M. Cousens
Keyword(s):  
New Zealand ◽  
North America ◽  
West Coast ◽  
Congeneric Species ◽  
The West ◽  
The Past ◽  
The North ◽  
Cakile Maritima ◽  
Cakile Edentula ◽  
North And South

AbstractOn the west coast of North America and in Australia, there have been parallel cases of sequential invasion and replacement of the shoreline plant American sea-rocket by European sea-rocket. A similar pattern has also occurred in New Zealand. For 30 to 40 yr, from its first recording in 1921, American sea-rocket spread throughout the eastern coastlines of the North and South Islands of New Zealand. European sea-rocket has so far been collected only on the North Island. From its first collection in 1937, European sea-rocket spread to the northern extremity of the island by 1973, and by 2010, it had reached the southernmost limit. In the region where both species have occurred in the past, American sea-rocket is now rarely found. This appears to be another example of congeneric species displacement.

Note on the Occurrence of Dayia navicula (J. de C. Sowerby) in the Lower Ludlow Rocks of Shropshire

1939 ◽  
Vol 76 (8) ◽  
pp. 360-361 ◽  
Author(s):  
J. Shirley
Keyword(s):  
Thin Layer ◽  
The West ◽  
West Side ◽  
Great Thickness ◽  
Railway Line ◽  
North East ◽  
The North ◽  
North Side ◽  
Large Numbers ◽  
Type Area

In the type area the Ludlow Rocks generally have been divided into Lower Ludlow Shales, Aymestry Limestone, Dayia Shales and Whitcliffe Flags in upward sequence. The Dayia Shales are characterized by the presence of enormous numbers of Dayia navicula (J. de C. Sowerby). This preponderance of D. navicula in the shales immediately above the Aymestry Limestone has caused a tendency to regard beds in other localities containing this fossil as being on the same stratigraphical horizon in spite of the character of the accompanying fauna. In two recent papers on the Ludlow Rocks of the Welsh Borderland (Straw, 1937, and Earp, 1938) it has been shown that D. navicula ranges through at least 3,000 feet of strata, occurring commonly throughout this great thickness and outlasting more than one change of fauna. Although, in this area, the brachiopod ranges from the zone of Monograptus nilssoni into the Upper Ludlow it has not hitherto been recorded below the Aymestry Limestone in Shropshire. This gap in our knowledge is now filled by the discovery of specimens in Lower Ludlow Shales exposed in a small quarry 40 yards north-east of Stokewood Cottage, which is on the west side of the railway line a little over a mile south of Craven Arms. The quarry shows about 15 feet of nodular shales with thin limestone seams. The commonest fossils are Chonetes laevigata (J. de C. Sowerby), C. minima (J. de C. Sowerby), and Stropheodonta filosa (J. de C. Sowerby) which occur in large numbers on some of the bedding surfaces. Other fossils are Stropheodonta euglypha (Dalman), Delthyris sp., Orthoceras sp., Dalmanites sp., and a plectambonitid. Dayia navicula seems to be confined to a thin layer on the north side of the quarry. Graptolites referable to Monograptus cf. chimaera occur fairly commonly. About 400 yards in a south-easterly direction another small quarry exposes Conchidium Limestone which is about 170 feet stratigraphically above the beds in the first quarry.

scholarly journals Last Cretaceous Geology of Taranaki Basin, New Zealand

2021 ◽  
Author(s):  
◽  
Glenn Paul Thrasher
Keyword(s):  
New Zealand ◽  
Late Cretaceous ◽  
Coastal Plain ◽  
New Caledonia ◽  
Strike Slip ◽  
Source Rocks ◽  
Petroleum Exploration ◽  
Petroleum Reservoir ◽  
The North ◽  
Potential Source Rock

<p>Taranaki Basin is a large sedimentary basin located along the western side of New Zealand, which contains all of this countries present petroleum production. The basin first formed as the late-Cretaceous Taranaki Rift, and the first widespread sediments are syn-rift deposits associated with this continental rifting. The Taranaki Rift was an obliquely extensional zone which transferred the movement associated with the opening of the New Caledonia Basin southward to the synchronous Tasman Sea oceanic spreading. Along the rift a series of small, en-echelon basins opened, controlled by high-angle normal and strike-slip faults. These small basins presently underlie the much larger Taranaki Basin. Since the initial rift phase, Taranaki Basin has undergone a complex Cenozoic history of subsidence, compression, additional rifting, and minor strike-slip faulting, all usually involving reactivation of the late-Cretaceous rift-controlling faults. One of the late-Cretaceous rift basins is the Pakawau Basin. Rocks deposited in this basin outcrop in Northwest Nelson as the Pakawau Group. Data from the outcrop and from wells drilled in the basin allow the Pakawau Group to be divided into two formations, the Rakopi Formation and the North Cape Formation, each with recognizable members. The Rakopi Formation (new name) is a sequence of terrestrial strata deposited by fans and meandering streams in an enclosed basin. The North Cape Formation is a transgressive sequence of marine, paralic and coastal-plain strata deposited in response to regional flooding of the rift. The coal-measure strata of the Rakopi Formation are organic rich, and are potential petroleum source rocks where buried deeply enough. In contrast, the marine portions of the North Cape Formation contain almost no organic matter and cannot be considered a potential source rock. Sandy facies within both formations have petroleum reservoir potential. The Rakopi and North Cape formations can be correlated with strata intersected by petroleum exploration wells throughout Taranaki Basin, and all syn-rift sediments can be assigned to them. The Taranaki Rift was initiated about 80 Ma, as recorded by the oldest sediments in the Rakopi Formation. The transgression recorded in the North Cape Formation propagated southwards from about 72 to 70 Ma, and the Taranaki Rift remained a large marine embayment until the end of the Cretaceous about 66.5 Ma. Shortly thereafter, a Paleocene regression caused the southern portions of Taranaki Basin to revert to terrestrial (Kapuni Group) sedimentation. The two distinct late Cretaceous sedimentary sequences of the Rakopi and North Cape formations can be identified on seismic reflection data, and the basal trangressive surface that separates them has been mapped throughout the basin. This horizon essentially marks the end of sedimentation in confined, terrestrial subbasins, and the beginning of Taranaki Basin as a single, continental-margin-related basin. Isopach maps show the Rakopi Formation to be up to 3000m thick and confined to fault- controlled basins. The North Cape Formation is up to 1500m thick and was deposited in a large north-south embayment, open to the New Caledonia basin to the northwest. This embayment was predominantly a shallow-marine feature, with shoreline and lower coastal plain facies deposited around its perimeter</p>

The Ruin at Thésée

Antiquity ◽  
1955 ◽  
Vol 29 (114) ◽  
pp. 102-106
Author(s):  
R. M. Butler
Keyword(s):  
The West ◽  
Main Road ◽  
Railway Line ◽  
The North ◽  
Large Size ◽  
North Bank ◽  
Road Following ◽  
The Village

The aim of this note is to bring to the attention of English readers a Roman building of large size, whose impressive ruins are well preserved, but whose purpose is uncertain and existence little known.The Roman road from Tours to Bourges ran along the north bank of the river Cher and for much of its length is followed by the modern N76. Two settlements or posting-stations lying on this road and marked on the Peutinger map under the names Gabris and Tasciaca can be located at the villages of Giévres and Thésée respectively. At this latter place, otherwise called Thézée or Tézée, 31 miles east of Tours, the main road, following the course of the Roman route, runs close beside the river, with the railway line separating them and low, bare hills rising immediately to the north. The towns of Montrichard to the west and St. Aignan on the east are respectively 4 and 5 miles away, and the village lies in the Loir-et-Cher département.

The Shaugh Moor Project: First Report

1979 ◽  
Vol 45 ◽  
pp. 1-33 ◽  
Author(s):  
G. J. Wainwright ◽  
A. Fleming ◽  
K. Smith
Keyword(s):  
Coastal Plain ◽  
Deciduous Forest ◽  
The South ◽  
Molten Material ◽  
The West ◽  
Central Mass ◽  
Climatic Trends ◽  
North East ◽  
The North ◽  
River Valleys

Viewed from the south Devon littoral with its series of good harbours the dark bulk of Dartmoor is clearly visible across the flat coastal plain. It is the largest of the five granite masses that provide a spine to the south-west English peninsula (Dartmoor, Bodmin Moor, Hensbarrow, Carnmenellis and Penwith) that were formed by the consolidation of molten material. The 500 square kilometres of the Moor form an undulating upland up to 600 m OD on the north-east side, where the greatest elevations occur. In the southern parts of the Moor the rolling tableland is 300 m to 420 m high—modern cultivation tends to cease at the 300 m contour, that is broken by numerous upland valleys and the eroded remains of tors. Today this expanse of moorland is bleak and treeless except in river valleys at the rim of the granite escarpment, although patches of contorted oak woodland survive at Piles' Wood on the River Erme, Wistman's Wood on the West Dart and Black Tor Beare on the West Okement. Pollen analyses have shown, however, that up to a height of about 360 m Dartmoor was probably covered by a deciduous forest dominated by oak that was gradually eroded by climatic trends and human activity (e.g. Simmons, 1969). It is from this central mass that the rivers of south Devon diverge. The wide upland valleys of the Tavy, Plym, Yealm, Erme, Avon and Dart plunge through characteristic deep wooded gorges near the southern granite escarpment into the South Hams and around this border modern settlement—numerous villages and a few towns are situated.

First record of the Australian longfinned eel, Anguilla reinhardtii, in New Zealand

1996 ◽  
Vol 47 (8) ◽  
pp. 1037 ◽  
Author(s):  
DJ Jellyman ◽  
BL Chisnall ◽  
LH Dijkstra ◽  
JAT Boubee
Keyword(s):  
New Zealand ◽  
West Coast ◽  
Dna Markers ◽  
First Record ◽  
Anecdotal Evidence ◽  
The West ◽  
The North ◽  
Waikato River

Anguilla reinhardtii has been identified by vertebral counts and DNA markers, from a sample of 27 individuals (364-790 mm), within eight consecutive year classes caught by commercial eel fishers in the Waikato River, North Island, New Zealand. There is anecdotal evidence that A. reinhardtii has been present in small numbers in New Zealand for at least 25 years, although its incidence in commercial catches is thought to be increasing. The present known distribution covers approximately 500 km of latitude along the top half of the west coast of the North Island.

The phonemes of New Zealand English

1966 ◽  
Vol 11 (2) ◽  
pp. 79-82 ◽  
Author(s):  
L. G. Kelly
Keyword(s):  
New Zealand ◽  
West Coast ◽  
Industrial Revolution ◽  
Gold Rush ◽  
The South ◽  
The West ◽  
Social Differences ◽  
Free Church ◽  
The North ◽  
English Society

The New Zealand accent belongs to the British group of English accents. There are three main divisions: General New Zealand, which is spoken in most parts of the country, and the accents of Otago, in the south of the South Island, and on the West Coast of the South Island. The three divisions follow the original pattern of settlement. In the North Island, settlement was directed by the New Zealand Company, which founded Auckland and Wellington in 1840; other settlements followed in the late 1840s. In the South, the Anglican Church founded Christchurch and Nelson in the early 1850s. These settlements had the common aim of reproducing English society as it existed in the south of England and drew most of their settlers from persons dispossessed by the Industrial Revolution. The difficulties of life in early New Zealand effectively levelled out social differences, with important effects on the language. Otago was founded in 1848 by the Scottish Free Church. The West Coast was not settled until the Gold Rush of the 1860s attracted miners from the goldfields of Victoria and California. Since that time there has been considerable immigration from the British Isles, at first a mere trickle from Europe and then a flood of Central European refugees after the Second World War. In general the willingness of the average New Zealander to travel for reasons of work or promotion has prevented the growth of regional accents; but the West Coast and Otago tend to keep to themselves, isolated by rough country and their own sense of community.

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