Things To Do
Glenmac Farmstay is located close to Kurow and Duntroon, and is part of the lower Waitaki Valley, which is a popular holiday area for New Zealand families due to the long, hot summer days and relaxed, countryside environment.
Glenmac Farmstay is located close to Kurow and Duntroon, and is part of the lower Waitaki Valley, which is a popular holiday area for New Zealand families due to the long, hot summer days and relaxed, countryside environment.
Oamaru is the 'capital' of the Waitaki District, however the Waitaki Valley is not only home to Kurow, but to some other fabulous rural townships that link visitors to Ohau, Mt Cook/Aoraki and other exciting routes. Each township features some wonderful attractions.
The Waitaki district is located in the centre of the South Island and is home to lush valleys, majestic mountains, pristine azure lakes, exciting rivers, New Zealand wildlife and breathtaking scenery, making it the ideal holiday spot for outdoor pursuits or pure relaxation.
The Waitaki Valley boasts a stunning natural environment that provides a huge amount of opportunities for outdoor enthusiasts to enjoy a genuine Kiwi outdoor holiday. No matter what your level of fitness or experience, there are plenty of hikes, bike tracks and walks.
Billowing clouds of gas, steam and ash are spewing out from the crater and you hesitate to move. An explosion seems imminent but the guide appears relaxed and in control.
Suddenly, as you look upwards you realize the entire roof of the cavern is a mass of ghostly pale green twinkling lights, so densely packed together that it resembles the Milky Way galaxy.
The track winds through a 'moonscape' of bizarre lava sculptures and up onto the shoulder of a towering volcanic cone, draped with a skirt of shifting cinders. Onward it goes, past red cliffs, active geothermal areas, silent emerald and blue lakes.
The Waimangu Cauldron steams away at a seething 53° Centigrade as you stroll downhill past Frying Pan Lake, the world's largest hot spring. Nearby is Inferno Crater, an inverted cone with strangely fluctuating water levels and a swirling head of steam.
It takes some mental agility to visualise just how the Dart Valley looked 18,000 years ago, at the peak of the last ice age, when the formidable Dart Glacier gouged Lake Wakatipu down to bedrock.
The pancake-like columns of rock are drenched in spray, highlighting the curious stylobedding process that weathers these layers of limestone seabed strata, stripping off the softer, less compacted areas, to leave the tottering towers.