Charles William Wilson,
1911 Encyclopedia Britannica
(1911)
“ On the north and west the slopes of Great Ararat are covered with glittering fields of unbroken névé. The only true glacier is on the north-east side, at the bottom of a large chasm which runs into the heart of the mountain. The great height of the snow-line, 14,000 ft., is due to the small rainfall and the upward rush of dry air from the plain of the Araxes. The middle zone of Ararat, 5000–11,500 ft., is covered with good pasture, the upper and lower zones are for the most part sterile. ”
