The Kyzylompol Range () is a mountain range in the Inner Tian Shan of Kyrgyzstan. It forms the eastern continuation of the Kyrgyz Ala-Too Range and lies west of the Issyk-Kul Basin. The range is long and wide. Its mean elevation is about 2,950 m, and its highest point reaches 3,183 m.
The range is composed mainly of Paleozoic syenite, granite-syenite, granite and other rocks. Remnants of ancient denudation surfaces occur along its crest. The slopes have gradients of 25–38° and are dissected by gullies and small valleys. To the west, the range gradually decreases in elevation and passes into Kubaky Pass, while to the east it descends into the Issyk-Kul Basin.
Dry-steppe landscapes predominate on the northern slopes, semi-desert landscapes on the southern slopes, and steppe landscapes in the western part.
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