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The following is a list of historic hotels in the New Zealand South Island Region of Otago. Otago, which during the late nineteenth century was New Zealand's richest province (thanks to the Otago gold rush has a wealth of historic buildings, many of them originally dedicated to the accommodation and hospitality trade.
The restaurant opened on October 8, 1990, in Shenzhen's special economic zone. The South China Morning Post reported that on its opening day, the unique McDonald's received over 40,000 customers ...
Mount Ngauruhoe from the blue sofa in the sitting area. In 1923, the newly established Tongariro National Park Board investigated a site for a 100-bed hostel in order to encourage tourists to visit the newly formed park, but it was not until 1925 that New Zealand Government, via the National Park Board, followed up this initiative by offering to lease land and lend up to £40,000 to any ...
Ōpārara Arch is the largest natural rock arch in the southern hemisphere. [2] An old sign at the end of the walking track inside the arch lists the measurements as 200m long, 49m wide, and 37m high., [3] however, the New Zealand Department of Conservation's measurements put it at 219m long, up to 79m wide, and 43m high.
Millbrook Resort is a luxury resort near Queenstown, New Zealand. It is located 4 kilometres to the west of the historic gold-mining town of Arrowtown . The resort covers 650 acres of the Wakatipu Basin - a glacial valley bordered by the Crown Range , The Remarkables and Lake Wakatipu .
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.
Eichardt‘s Private Hotel is located on the corner of Marine Parade and Ballarat Street, Queenstown, New Zealand, on the shores of Lake Wakatipu. Eichardt’s is a significant local landmark, and is listed as a Category Two historic place by the Historic Places Trust. [1] Eichardt's building in Queenstown
New Zealand's geomorphology is formed through an interaction between uplift, erosion and the underlying 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 joints or faults in the rock-mass. [ 1 ]
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