The island of Taiwan is situated at the intersection of two tectonic plates – the Eurasian Plate and the Philippine Sea Plate. Even as “recently” as the late Paleozoic (some 250 million years ago), the land here was still but a sedimentary seabed layered with silt and sand. As the two plates began pressing against each other, the land buckled, bent, and created the landscape – 165 mountains higher than above sea level on a relatively small island (38th largest in the world).