| Kon | |
| Other Name: | Көң |
| Source1: | Zeldiadyr |
| Source1 Coordinates: | 49.3703°N 67.735°W (Zhaksykon) |
| Source1 Elevation: | ca 700m (2,300feet) |
| Mouth: | Kulanotpes |
| Mouth Coordinates: | 50.1914°N 69.5008°W |
| Mouth Elevation: | 320m (1,050feet) |
| Progression: | Kulanotpes→Lake Tengiz |
| Subdivision Type1: | Country |
| Subdivision Name1: | Kazakhstan |
| Length: | 160km (100miles) |
| Discharge1 Avg: | 0.82m3/s |
| Basin Size: | 4050km2 |
| Pushpin Map: | Kazakhstan |
| Pushpin Map Caption: | Mouth location in Kazakhstan |
The Kon (Kazakh: Көң; Russian: Кон) is a river in the Nura District, Karaganda Region, Kazakhstan.[1] It has a length of and a drainage basin of 4050km2.[2]
The Kon is the most important tributary of the Kulanotpes, followed by the long Sonaly. 2.5km (01.6miles) to the south of its mouth lies Kulanotpes village.[1] [2]
The Kon river originates in the Zeldiadyr, a range of mountains located by the eastern part of the Ulytau Range, one of the main mountain groups of the Kazakh Uplands. In its upper course the river is known as Zhaksykon and flows within a narrow valley. It heads first roughly eastwards along the feet of the southern slopes of the Zeldiadyr, bending northeastwards at the eastern end of the range, while still as the Zhaksykon. Further downriver it bends northwards and is joined by the Zhamankon from the right, being known as the Kon after the confluence. The river flows then roughly northwards within a 2km (01miles) to 3km (02miles) wide floodplain all along its course, sometimes dividing into channels as a braided river. In its last stretch the Kon forks into two and joins the left bank of the Kulanotpes.[2] [1]
The river is surrounded by highland steppe. Its channel is often bound by not well-defined banks. North of the confluence of the Zhaksykon and Zhamankon the river has no significant tributaries.[1] The annual water flow of the Kon is 53000000m2 and the seasonal fluctuation in water volume is very pronounced. In the spring the water level may rise between 4m (13feet) to 5m (16feet) and in the summer the river may stop flowing and splits into disconnected pools. The average duration of the dry period is 127 days, but in years of severe drought it may reach 250 days. Following the melting of the surrounding snows in the spring, the river water is fresh, but has a tendency to become brackish, with an increased mineralization especially towards the autumn.[3]
