At the end of the end of the world In the furious fifties, 100 miles east of Cape Horn, at the end of Tierra del Fuego, the 65 km long Staten Island rises from an ocean of whitecaps and the giant antarctic
swell. A tortured geography Staten Island is evidence of the continental drift fragmenting the earth's crust many millions of years ago. As the last seed of the Andes Cordillera, the island possesses
a tortuous topography. A particularly inhospitable island The island's climate is cold, very wet and with extreme winds. The average temperature is between 0 and 5 °C. Precipitation is in the form of rain or snow and is nearly daily (25 days a month on average), yearly rainfall is close to 4 meters! Moisture and fog levels are very high. The island can totally disappear in the clouds descending to sea level. Close to Cap Horn the island has the same conditions: Successive low pressures and exceptionally violent gales. An exuberant vegetation. The vegetation influenced by the humid climate and the nearly daily rain is abundant and exuberant. Trees are abused by the violent winds blowing nearly always in the same direction. They are tiny and grow nearly horizontal like a banner! Fallen trees practically don't rot, their trunks whitening and accumulating in an entanglement rendering every move on the island extremely complicated. Wildlife The endemic wildlife is composed of penguins, seals, otters, albatrosses, seagulls, petrels, ducks. The Indians living in Tierra del Fuego called it "Land of Plenty". The
accounts of explorers mention that they had to reduce sails to slow their vessels because of the crowded waters! There is also the wildlife introduced by explorers. They used to transport livestock to set free on the islands they encountered in order to have fresh food for their next
passage. During the XIXth century hunting (seals, otters, penguins) caused wildlife depletion. |