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The Whale Trail is a shared-use long-distance trail under construction from Picton to Kaikōura in the South Island of New Zealand. When completed, the trail will provide a route between Picton, Blenheim , Seddon , Ward , Kekerengu , Clarence and Kaikōura.
Some of the free software mentioned here does not have detailed maps (or maps at all) or the ability to follow streets or type in street names (no geocoding). However, in many cases, it is also that which makes the program free (and sometimes open source [ 1 ] ), avoid the need of an Internet connection, [ 2 ] [ 3 ] [ 4 ] and make it very ...
AllTrails is a fitness and travel mobile app used in outdoor recreational activities. This app is commonly used for outdoor activities such as hiking, mountain biking, climbing and snow sports. The service allows users to access a database of trail maps, which includes crowdsourced reviews and images.
Wikiloc is a website, launched in 2006, [2] [3] [4] containing GPS trails and waypoints that members have uploaded. [3] This mashup shows the routes in frames showing Google Maps (with the possibility to show the layers of World Relief Map (maps-for-free.com), OpenStreetMap, the related OpenCycleMap, USGS Imagery Topo Base Map and USGS Topo Base Map).
Kaikoura Island (formerly known as Selwyn Island) lies in an irregularly-shaped bay on the western side of Great Barrier Island in the Hauraki Gulf in New Zealand, 90 km (56 mi) north east of Auckland. Kaikoura Island is the seventh largest island in the Hauraki Gulf.
Map of the Tour Aotearoa bikepacking route. Tour Aotearoa is an annual cycle tour event [1] and cycling route in New Zealand. [2] The route travels 3,000 kilometres (1,900 mi) from Cape Reinga to Bluff.
Wave cut platform formation. The Kaikōura Peninsula is located on the east coast of the South Island of New Zealand. Geologically the peninsula consists of an asymmetrical anticline bounded on either side by two synclines, the axis of which strikes northeast–southwest. [3]
The Kaikōura Canyon is deeply incised into the narrow, tectonically active, continental margin and is the main sediment source of the 1,500 km (930 mi) long Hikurangi Channel, which supplies turbidites to the Hikurangi Trough, as well as to low parts of the oceanic Hikurangi Plateau, and to the edge of the southwest Pacific Basin.