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Armenia, Travels and Studies (Volume 1 of 2)

Note 2 — Chapter XIII · THE HEART OF ARARAT

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It is a melancholy reflection that nothing is lasting—that the strength of the earth withers and the strength of the human body, that faith dies and the closest friendships dissolve. In the world of sense Time is all-powerful, and nothing escapes destruction at his hands.2 This painful lesson is written with terrible emphasis on the fabric of Ararat, where it fronts the historic river and the historic plains. Another earthquake, and the massive roof may tumble headlong into the abyss which now yawns beneath its cornice of snow. I have already observed that Herrmann Abich was able to remark a lateral fissure between the two highest elevations in the surface of the crown of the dome. He suggests that this fissure may have been caused by the convulsion of 1840, to which the present configuration of the chasm is due.3 It would therefore appear that Time has already taken a decisive step towards the overthrow of the uppermost portion of the cone. The chasm itself and the subsidence of the flank of the mountain date from an epoch beyond the range of history. Tournefort, who visited Ararat in 1701, presents us with such a vivid picture of the rent side of the giant, that one cannot doubt that the essential features of the chasm existed in his day.4 The little monastery of St. Jacob, which, prior to the catastrophe of 1840, stood within the recesses of the gulf, probably occupied the same site when it was first erected in the early Christian times. The reader may not be acquainted with the story of the catastrophe, and may like to learn or to recall it in this place.

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