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- Afon Hepste - Wikipedia
Afon Hepste (Welsh pronunciation: [ˈhɛpstɛ]) is a river in Powys, Wales, though partly forming the county's border with Rhondda Cynon Taf It runs wholly within the Brecon Beacons National Park
- Afon Hepste, Brecon Beacons National Park, Powys - UK SOUTHWEST
The Afon (River) Hepste flows for five miles, starting south of Fan Fawr in the middle of Brecon Beacons National Park and meeting the larger Afon Mellte, a third of a mile beyond one of the most spectacular waterfalls in the park, Sgwd yr Eira, Fall of Snow
- Afon Hepste | South | Wales | Rivers - The UK Rivers Guidebook
Portaging on river right, you eventually get back to the river just before it enters the River Mellte Perhaps the best paddling is still to come, look at the Mellte guide for more information
- River Hepste - Wikishire
The River Hepste is a Brecknockshire river wholly within the Brecon Beacons National Park Its headwaters, the Afon y Waun, Nant y Cwrier and Nant Hepste Fechan, rise on the Old Red Sandstone dip-slopes of Fforest Fawr and combine to form the Hepste near the farmstead of Hepste Fechan
- Sgwd yr Eira waterfall, Bannau Brycheiniog National Park, Wales
Well-marked trails connect this waterfall to others along the River Hepste, making it a popular stop on longer hikes Above the valleys, the landscape opens into rolling moorland and long ridgelines where upland paths are shaped by wind and changing weather
- Hepste | Current River Conditions
Hepste: get real-time water levels, flow, and temperature data Ideal for fishing and kayaking – Live gauge updates from multiple sites
- Ystradfellte Waterfalls Walk Walk, Brecon Beacons
From here careful navigation takes you off the "Four Waterfalls Walk" to Sgwyd yr Elra falls on the River Hepste, which is crossed If in doubt return to the "Four Waterfalls Walk" and complete the loop back to the start
- Afon Hepste, Powys | GeoGuide
The Afon Hepste downstream of Hepste Bridge provides an excellent example of the geological controls on river development It is characterized in its upper reaches by a dry stream course over areas of Carboniferous limestone and in the lower part by waterfalls
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