There are mountains, and there is the Matterhorn.
The Matterhorn was the last great Alpine peak to be climbed
and its first ascent in 1865 marked the end of the golden age of
alpinism. Seven men reached the summit but four died on the
way back. The triumph and tragedy of this feat is the epitome of
man's desire to explore, to go beyond the limit. A reminder of
how great and how small we are at the same time.
The Matterhorn is a product of geological processes that
transcend our concept of time. It was born from the remnants
of an enormous African rock mass which originated more than
250 million years ago. This mass was pushed northwards
colliding with the European continental plate, forcing its way
upwards and resulting in alpine folding 100 million years ago. It
reached its maximum heights 30 million years ago, modeled by
natural erosion from the top to the bottom, and finally acquired
its characteristic pyramidal shape over the last 2.6 million years.
The Matterhorn that is rising to the sky today, although graceful
and uniquely formed, is just a majestic ruin, only a fragment of
an eroded mountain. It is subject to wear caused by erosion and
weathering and it will eventually round off and disappear
forever. In the long term, plate tectonics will finish the job. The
geological clock will reset all over again and a new Matterhorn
will emerge somewhere else in 50-300 million years.
Will humans be around to climb those mountains?