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| | Fox and Franz Josef Glaciers, New Zealand |
 | | A visit to the Fox and Franz Josef glaciers gives a good understanding of erosion by moving ice because it is happening right now, near sea level, accessible to the unfit, at a comfortable temperature, close to excellent accommodation and tourist buses. |
 | | The Southern Alps of New Zealand are elevated by tectonic compression along the alpine fault. |
 | | When first explored by Europeans, (A.P. Harper and Charlie Douglas, 1865), the glacier was probably at a new peak after the little ice age, There is a lag period between changes in climate and position of the glacier's terminal, because ice flow is slow. |
| members.tripod.com /NZPhoto/south/04Glaciers.htm (1138 words) |
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