From the archive record
Truly the 'Abode of the Snow', the mighty Himalayas that spread across from northern most India to Tibet and Bhutan and parts in China do offer out of the world views of a frozen landscape. The white snow is almost blinding in the day if the sun decides to show up. The Himalayas are among the youngest mountain ranges on the planet and consist mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, their formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision. During the Upper Cretaceous, about 70 million years ago