With Spectacular glaciers, picturesque fiords, rugged mountains, vast plains, rolling hillsides, subtropical forest, volcanic plateau, miles of coastline with gorgeous sandy beaches, Thats The New Zealand. Lying in the south-west 
Pacific, New Zealand consists of two main islands - the North Island and the South Island. In addition, Stewart Island and many smaller islands lie offshore. The North Island has a 'spine' of mountain ranges running through the middle, with gentle rolling farmland on both sides. The central North Island is dominated by the Volcanic Plateau, an active volcanic and thermal area. The massive Southern Alps form the backbone of the South Island. To the east of the Southern Alps is the rolling farmland of Otago and Southland, and the vast, flat Canterbury Plains. New Zealand sits on two tectonic plates - the Pacific and the Australian. Fifteen of these gigantic moving chunks of crust make up the Earth's surface. The North Island and some parts of the South Island sit on the Australian Plate, while the rest of the South Island sits on the Pacific. New Zealand with some spectacular geothermal areas and relaxing hot springs, as well as providing electricity and heating in some areas. About a fifth of the North Island and two-thirds of the South Island are mountains. The existence of a ‘spine’ of mountain ranges throughout New Zealand is also due to the movement of the earth’s tectonic plates. Stretching from the north of the North Island to the bottom of the South, these mountains are caused by the collision of the Australian and Pacific Plates.
About a fifth of the North Island and two-thirds of the South Island are mountains. The existence of a ‘spine’ of mountain ranges throughout New Zealand is also due to the movement of the earth’s tectonic plates. Stretching from the north of the North Island to the bottom of the South, these mountains are caused by the collision of the Australian and Pacific Plates. Over millions of years, alluvial deposits (eroded from the mountains by rivers) formed the vast Canterbury Plains in the South Island and a number of smaller plains in the North. These alluvial plains contain some of New Zealand’s most fertile and productive farmland. New Zealand’s Southern Alps have a number of glaciers, the largest being Tasman glacier, which you can view by taking a short walk from Mount Cook village. New Zealand’s most famous glaciers are the Franz Josef and Fox on the South Island’s West Coast. Gouged out by moving ice over thousands of years, these spectacular glaciers are easily accessible to mountaineers and hikers. Over thousands of years, the process of subduction has seen parts of the New Zealand landscape become submerged. Visit and Cruise to Paradise island the New Zealand.
Pacific, New Zealand consists of two main islands - the North Island and the South Island. In addition, Stewart Island and many smaller islands lie offshore. The North Island has a 'spine' of mountain ranges running through the middle, with gentle rolling farmland on both sides. The central North Island is dominated by the Volcanic Plateau, an active volcanic and thermal area. The massive Southern Alps form the backbone of the South Island. To the east of the Southern Alps is the rolling farmland of Otago and Southland, and the vast, flat Canterbury Plains. New Zealand sits on two tectonic plates - the Pacific and the Australian. Fifteen of these gigantic moving chunks of crust make up the Earth's surface. The North Island and some parts of the South Island sit on the Australian Plate, while the rest of the South Island sits on the Pacific. New Zealand with some spectacular geothermal areas and relaxing hot springs, as well as providing electricity and heating in some areas. About a fifth of the North Island and two-thirds of the South Island are mountains. The existence of a ‘spine’ of mountain ranges throughout New Zealand is also due to the movement of the earth’s tectonic plates. Stretching from the north of the North Island to the bottom of the South, these mountains are caused by the collision of the Australian and Pacific Plates.About a fifth of the North Island and two-thirds of the South Island are mountains. The existence of a ‘spine’ of mountain ranges throughout New Zealand is also due to the movement of the earth’s tectonic plates. Stretching from the north of the North Island to the bottom of the South, these mountains are caused by the collision of the Australian and Pacific Plates. Over millions of years, alluvial deposits (eroded from the mountains by rivers) formed the vast Canterbury Plains in the South Island and a number of smaller plains in the North. These alluvial plains contain some of New Zealand’s most fertile and productive farmland. New Zealand’s Southern Alps have a number of glaciers, the largest being Tasman glacier, which you can view by taking a short walk from Mount Cook village. New Zealand’s most famous glaciers are the Franz Josef and Fox on the South Island’s West Coast. Gouged out by moving ice over thousands of years, these spectacular glaciers are easily accessible to mountaineers and hikers. Over thousands of years, the process of subduction has seen parts of the New Zealand landscape become submerged. Visit and Cruise to Paradise island the New Zealand.