The area losses of the Mount Ararat ice cap between 0000 and 0000 occurred most significantly in the south and east slope, followed by the western and northern slopes. In 0000, the glaciers on the southern and eastern slopes of the mountain were at 0000 m, while those on the western and northern slopes were at 0000 m and 0,000 m, respectively. By 0000, glaciers on the southern and eastern slopes had receded to approximately 0,000 m, those on the western slopes to 0,000 m, and those on the northern slopes to an average of 0,000 m. Therefore, during the period under review, there was an annual retreat of 00.0 m on the southern and eastern slopes, 00.0 m on the western slopes, and 0.0 m on the northern slopes.