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- River_Haffes abstract "The Afon Haffes is a river in Powys, Wales and is wholly contained within the Brecon Beacons National Park.Its headwaters rise on the southern and western slopes of Fan Hir at the eastern edge of the Black Mountain and the river joins the River Tawe at Glyntawe after a short and steep south-eastward descent of 3 km / 2 miles.Cwm Haffes is a trench which has been incised into the glacial till left by the glaciers of the last ice age along the geological boundary between the Old Red Sandstone rocks to the north and the Carboniferous Limestone rocks to the south. At the head of the incised valley is Sgwd Ddu (translated from Welsh as 'black fall').The river forms two distributaries as it enters the River Tawe on account of its large bedload of boulders derived from the glacial material through which it has cut.".
- River_Haffes wikiPageExternalLink search.php?i=5973874.
- River_Haffes wikiPageID "20936517".
- River_Haffes wikiPageRevisionID "580866015".
- River_Haffes hasPhotoCollection River_Haffes.
- River_Haffes subject Category:Black_Mountain,_Wales.
- River_Haffes subject Category:Fforest_Fawr.
- River_Haffes subject Category:Rivers_of_Powys.
- River_Haffes subject Category:Rivers_of_the_Brecon_Beacons_National_Park.
- River_Haffes point "51.8345 -3.6757".
- River_Haffes type BodyOfWater109225146.
- River_Haffes type PhysicalEntity100001930.
- River_Haffes type River109411430.
- River_Haffes type RiversOfPowys.
- River_Haffes type RiversOfWales.
- River_Haffes type Stream109448361.
- River_Haffes type Thing100002452.
- River_Haffes type YagoGeoEntity.
- River_Haffes type YagoPermanentlyLocatedEntity.
- River_Haffes type SpatialThing.
- River_Haffes comment "The Afon Haffes is a river in Powys, Wales and is wholly contained within the Brecon Beacons National Park.Its headwaters rise on the southern and western slopes of Fan Hir at the eastern edge of the Black Mountain and the river joins the River Tawe at Glyntawe after a short and steep south-eastward descent of 3 km / 2 miles.Cwm Haffes is a trench which has been incised into the glacial till left by the glaciers of the last ice age along the geological boundary between the Old Red Sandstone rocks to the north and the Carboniferous Limestone rocks to the south. ".
- River_Haffes label "River Haffes".
- River_Haffes sameAs m.05b54j0.
- River_Haffes sameAs Q7337480.
- River_Haffes sameAs Q7337480.
- River_Haffes sameAs River_Haffes.
- River_Haffes lat "51.8345".
- River_Haffes long "-3.6757".
- River_Haffes wasDerivedFrom River_Haffes?oldid=580866015.
- River_Haffes isPrimaryTopicOf River_Haffes.