| Pay-Khoy Range | |
| Other Name: | хребет Пай-Хой |
| Country: | Russia |
| Region Type: | Federal subject |
| Region: | Nenets Autonomous Okrug |
| Highest: | Morye-Iz |
| Elevation M: | 423 |
| Coordinates: | 69.4275°N 62.2089°W |
| Length Orientation: | NW/SE |
| Width Orientation: | NE/SW |
| Parent: | Urals |
| Range Coordinates: | 69.2036°N 62.6078°W |
| Geology: | Sandstone, marl, limestone and crystalline shale |
| Period: | Late Triassic - Early Jurassic. |
| Orogeny: | Cimmerian Orogeny |
| Map: | Russia Nenets Autonomous Okrug |
| Map Relief: | yes |
| Easiest Route: | From Amderma |
The Pay-Khoy Range[1] (Russian: хребет Пай-Хой) is a mountain range at the northern end of the Ural Mountains. It lies within the Nenets Autonomous Okrug.
The ridge is extended from northwest to southeast. It is located on the Yugorsky Peninsula, in the eastern part of the Nenets Autonomous Okrug. The ridge continues to Vaygach Island, thus separating the Barents Sea and the Kara Sea. The highest point of Pay-Khoy is the mountain of Moreiz (467m (1,532feet)).[2] The range separates the drainage basins of the (west, Barents Sea) and the Kara River (east, Kara Sea).
The areas around Pay-Khoy do not have permanent population. The closest permanent settlements are Amderma and Ust-Kara, Nenets Autonomous Okrug The range is located in the tundra, to the north of the tree line.
The Pay-Khoy range forms a curved orogen together with the Ural Mountains, Vaygach Island and the Novaya Zemlya archipelago. The Pay-Khoy and Novaya Zemlya are younger than the orogeny that formed the Ural mountains. They were formed during the Cimmerian Orogeny between the Late Triassic and Early Jurassic.[3]