The large Franz Josef Glacier, located on the West Coast of refreshed Zealands South island, descends to just 250 meters above ocean level amidst the verdancy of a temperate rainforest. The direct distance from Brisbane, Australia, to the glacier is approximately 2500 km.
Of entirely the accessible temperate glaciers in New Zealand, the Franz Josef Glacier is the steepest and fastest moving. piece of music many glaciers worldwide hire been retreating, the Franz Josef Glacier still flows almost to sea level, with a rainforest of ancient trees and other coniferous species.
This combination of ice and temperate rainforest is a ludicrous feature of New Zealands glacier country, and is an ecosystem found nowhere else in the world.
Running through Franz Josef is the Alpine Fault. Along this fault line, the Southern Alps have been pushed up, and continue to rise. The weather that flows on to the West Coast is agonistic to rise over the Southern Alps, thereby cooling and falling most of its moisture as rain and snow. This process causes up to 30 meters of snow to fall on the catchments area of the glacier, either year.
The glacier slides forward at rates up to 10 measure faster than most valley glaciers, presenting the visitor with a spectacular and unique view of ice caves and canyons.
THIS PAPER WAS EXTREMELY nearsighted AND SHOULD HAVE BEEN MORE DETAILED SO A person COULD GET A BETTER UNDERSTANDING ABOUT THE FRANZ JOSEPH GLACIER IN NEW ZEALAND AND THHE DISTANCE OF THE GLACIER FROM AUSTRALIA
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