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・ Stokes phenomenon
・ Stokes radius
・ Stokes Range
・ Stokes relations
・ Stokes River
・ Stokes shift
・ Stokes State Forest
・ Stokes stream function
・ Stokes Township
・ Stokes Township, Itasca County, Minnesota
・ Stokes Township, Logan County, Ohio
・ Stokes Township, Madison County, Ohio
・ Stokes Township, Minnesota
・ Stokes Township, Ohio
・ Stokes Township, Roseau County, Minnesota
Stokes Valley
・ Stokes Valley RFC
・ Stokes wave
・ Stokes' law
・ Stokes' law of sound attenuation
・ Stokes' paradox
・ Stokes' theorem
・ Stokes, North Carolina
・ Stokes-Lee House
・ Stokes-Mayfield House
・ Stokesay
・ Stokesay Castle
・ Stokesay Court
・ Stokesby with Herringby
・ Stokesdale Historic District


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Stokes Valley : ウィキペディア英語版
Stokes Valley

Stokes Valley, a major suburb of the city of Lower Hutt in the North Island of New Zealand, lies at the northeastern edge of the city seven kilometres northeast of the city centre. It occupies the valley of a small tributary of the Hutt River, called Stokes Valley Stream, which flows north to meet the main river close to the Taita Gorge. Stokes Valley was named after Robert Stokes, who formed part of the original survey team of 1840 commissioned to plan the city at Thorndon in Wellington.
Stokes Valley is a suburb in its own valley. It is partially separated from the main part of the city of Lower Hutt and is surrounded on all sides by densely forested hills.
Its cultural identity, very similar to that of the rest of Lower Hutt, has progressed (would jokingly disagree ) a long way from the ''"congregation of old sheelbacks and whalers, men-o'-wars men and seamen, lags and hard cases, living in tents and whares ... () heterogeneous mass of misguided humanity"''〔Otago Witness, our midland letter, Issue 2346, 9 February 1899, Page 24>〕 reported in 1855.
==Geology and early history==
It has been suggested that the valley was formed during the ice age 10,000–20,000 years ago by glacial scouring, but considering that the Hutt Valley and the greater Wellington area have experienced major tectonic uplifting it is possible that the valley was formed through major earthquakes and erosion.
According to tradition, Māori arrived in the Hutt Valley in about 1250 AD when the two sons of Whatonga, a Hawke's Bay chief, settled in the area and named the Hutt River ''Heretaunga'', after their old home.〔McLintock, A.H. (ed.) (1966) ''An Encyclopaedia of New Zealand.'' Wellington: New Zealand Government Printers.〕〔http://www.teara.govt.nz/en/1966/lower-hutt/1〕 Although Māori had lived in the Hutt Valley for almost 600 years prior to Europeans, there has been no evidence of Māori habitation in Stokes Valley and the closest iwi (tribe), located at Waiwhetu, say they never used the valley for any significant purpose before Europeans arrived. Stokes Valley was located at the junction of the claimed territory of three major Maori tribes, the Te Ati Awa who sold it to European settlers,〔http://www.teara.govt.nz/en/1966/te-puni-honiana/〕 Ngāti Toa, and the Ngāti Kahungunu, and for this reason it would have in all likelihood never have been inhabited. This partially explains an extreme willingness to include this land in the sale to the early settlers.〔Watts, M. & P. (1953). ''Stokes Valley... Through the Years.'' Wellington: Commercial Printing and Publishing Co.〕

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