| River Glen | |
|---|---|
 River Glen | |
  Location within Northumberland | |
| Location | |
| Country | United Kingdom |
| County | Northumberland |
| Physical characteristics | |
| Source | |
| • coordinates | 55°34′08″N 2°08′43″W / 55.5688°N 2.1454°W |
| Mouth | |
• coordinates | 55°35′11″N 2°02′20″W / 55.5865°N 2.0388°W |
| Length | 12 km (7.5 mi) |
| Discharge | |
| • location | Kirknewton |
| • average | 2.93 m3/s (103 cu ft/s) |
The River Glen is a seven mile long tributary of the River Till flowing through Northumberland, England. The College Burn and Bowmont Water, both flowing out of the Cheviot Hills, meet near Kirknewton to form the River Glen. The Glen flows past the small settlements of Yeavering, Lanton, Coupland, Akeld and Ewart, before joining the Till.[1]
- ^ "Glen from College Burn to Till". Catchment Data Explorer. Environment Agency. Retrieved 17 April 2016.