| Kulduk-Too | |
| Country: | Kyrgyzstan |
| Subdivision2 Type: | Regions |
| Subdivision2: | Batken Region |
| Subdivision3 Type: | Districts |
| Subdivision3: | Batken District |
| Elevation M: | 5016 |
| Coordinates: | 39.6833°N 78°W |
| Length Km: | 31 |
| Width Km: | 7-8 |
| Formed By: | shale, limestone, and conglomerate of Silurian and Carboniferous, and more rarely by granite and granodiorite |
| Map: | Kyrgyzstan |
Kulduk-Too (Kirghiz; Kyrgyz: Кулдук-Тоо) is a northern offspur of the Alay Range in the Batken Region of Kyrgyzstan. It is located between the valley of the river Sokh and that of its tributary Kojashkan.[1] It stretches from west to east, south of the Aydarken depression, and is connected in the east with the Kuruk-say Range. The length of the range is 31km (19miles), its width is NaNkm (-2,147,483,648miles). Its average height is NaNm (-2,147,483,648feet), and its highest point is 5016m (16,457feet).[1] The northern slope, long and gentle, gradually descends to Sokh river and Khaidarkan depression. The southern slope, short and steep, features great variations in altitudes. Both slopes are deeply dissected by tributaries of Sokh river. The range is composed of Silurian and Carboniferous rocks: (shale, limestone, and conglomerate) and more rarely by intrusive rock such as granite and granodiorite.[2]