In this article, the mountain system of Kyrgyzstan is examined as a unique geographical object that defines the hydrological, climatic, and cultural landscape of the region. Based on analysis of orographic data, glaciological studies, and historical evidence, the complex structure of the Tian Shan and Pamir-Alay is reconstructed, forming more than ninety percent of the republic's territory. Special attention is given to the highest peaks—the Pobeda Peak and Khan-Tengri, to glacier complexes, as well as to the processes that link the cryosphere with the water security of the entire Central Asian region.

РЫБАЛКО ПАВЕЛ СЕМЕНОВИЧ, МАРШАЛ БРОНЕТАНКОВЫХ ВОЙСК. ГЕРОЙ БЕРЛИНА И ПРАГИ

На гражданской службе

ЧЕРНЫЙ КОНТИНЕНТ В КАДРЕ И ЗА КАДРОМ (ИЗ КИНОЛЕТОПИСИ ВТОРОЙ МИРОВОЙ ВОЙНЫ)

Одиссея барона Унгерна

ВОСПОМИНАНИЯ. Очерки из моей жизни

ДВУХСОТЛЕТИЕ НАЧАЛА ВОЙНЫ ЗА НЕЗАВИСИМОСТЬ И СТОЛЕТИЕ РЕВОЛЮЦИИ 1910 года В МЕКСИКЕ

СТЕНТОН Ф. АНГЛО-САКСОНСКИЙ ПЕРИОД В ИСТОРИИ АНГЛИИ