Mells River is a topic that has captured the attention of people around the world. Since its emergence, it has generated great interest and debate in different areas, whether in politics, culture, science or society in general. This topic has been the subject of research and analysis by experts and academics, with the aim of understanding its impact and implications. Furthermore, it has aroused the interest of the general population, generating conversations and reflections on different platforms and discussion spaces. In this article we will explore Mells River in detail, analyzing its most relevant aspects and offering a broad and varied perspective on this topic.
Mells River | |
---|---|
Location | |
Country | England |
County | Somerset |
Cities | Gurney Slade, Mells, Great Elm, Frome |
Physical characteristics | |
Source | |
• location | Somerset, England |
• elevation | 2 m (6 ft 7 in) |
Mouth | River Frome |
• location | Frome, Somerset, England |
• coordinates | 51°14′50″N 2°19′14″W / 51.24722°N 2.32056°W |
Basin features | |
Tributaries | |
• right | Finger Stream, Whatley Brook, Nunney Brook |
The Mells River flows through the eastern Mendip Hills in Somerset, England. It rises at Gurney Slade and flows east joining the River Frome at Frome.
The river forms one of the boundaries of Mells Park, a country house estate in Mells. A few kilometres downstream it flows between the pre-Roman fortifications of Wadbury Camp to the north and Tedbury Camp to the south. The river flows through the western part of the Harridge Woods nature reserve.
Mells River also powered the Old Ironstone Works and several other mills set up by James Fussell III in 1744. It is now a 0.25 hectare biological Site of Special Scientific Interest, as it is used by both Greater and Lesser Horseshoe Bats.
Vobster Inn Bridge, which carries the lane over the Mells River, is dated 1764 and is Grade II listed. At Great Elm the Murtry Aqueduct, built around 1795, carried the Dorset and Somerset Canal over the river.
The river takes the outfall from Whatley Quarry. Downstream of the outfall is the Mells River Sink. This acts as a spring when the water table is high and as a sink into underground aquifers, through the Limestone, when the water table is low. Water tracing showed this to be part of an underground part of the river 2.5 kilometres (1.6 mi) long. Archaeological investigations found the remains of woolly rhinoceros bones and a 1st-century bronze brooch.