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Hay Bluff
Hay Bluff ( Welsh: ''Penybegwn'') is a prominent hill at the northern tip of the Black Mountains, an extensive upland massif which straddles the border between south-east Wales and England. The mountain sits at the point where the main northeast-facing escarpment of the Black Mountains meets the northwest facing escarpment, the next peak to the west being Twmpa. The flat summit of Hay Bluff which is marked by a triangulation pillar at a height of overlooks the middle Wye Valley and the book town of Hay-on-Wye. The hill is largely within the Welsh county of Powys though parts of its eastern flanks lie within the English county of Herefordshire. In 2024 a monolith similar to the one in Utah was found atop the hill. It is unknown who placed it there or for what purpose. Geology The base and indeed greater part of the hill is formed from mudstones of the St Maughans Formation whilst the upper part is formed from the sandstones and mudstones of the Senni Formation (formerly kno ...
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Black Mountains, Wales
The Black Mountains ( or sometimes ) are a group of hills on the England–Wales border. The Welsh part is larger and located in south-east Powys and north-west Monmouthshire, and the smaller English part is in western Herefordshire. The range may be roughly defined as those hills contained within a triangle defined by the towns of Abergavenny in the southeast, Hay-on-Wye in the north and the village of Llangors in the west. Other gateway towns to the Black Mountains include Talgarth and Crickhowell. The Welsh part of the Black Mountains is the easternmost of the four ranges of hills that comprise the Brecon Beacons National Park; they should not be confused with the westernmost, the similarly-named Black Mountain (range), Wales, Black Mountain. The range of hills is well known to walkers and ramblers for the ease of access and views from the many ridge trails, such as that on the Black Hill (Herefordshire), Black Hill in Herefordshire, at the eastern edge of the massif. Gospe ...
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Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ...
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Freedom To Roam
The freedom to roam, or everyone's right, every person's right or everyman's right, is the general public's right to access certain public or privately owned land, lakes, and rivers for recreation and exercise. The right is sometimes called the right of public access to the wilderness or the right to roam. In Austria, Belarus, Estonia, Finland, Iceland, Latvia, Lithuania, Norway, Scotland, Sweden, Switzerland and the Czech Republic, the freedom to roam takes the form of general public rights which are sometimes codified in law. The access is ancient in parts of Northern Europe and has been regarded as sufficiently fundamental that it was not formalised in law until modern times. However, the right usually does not include any substantial economic exploitation, such as hunting or logging, or disruptive activities, such as making fires and driving offroad vehicles. In countries without such general rights, there may be a network of rights of way, or some nature reserves with foot ...
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Longtown, Herefordshire
Longtown is a linear village and parish in Herefordshire, England. The parish includes the village of Clodock and had a population in mid-2010 of 543, increasing to 620 at the 2011 Census. Location Longtown is located north east of Abergavenny and south west of Hereford on the eastern edge of the Black Mountains, Wales, part of the Brecon Beacons National Park. The extensive Hatterall Ridge lies about a mile to the west of the village, and the Black Hill (Herefordshire) two miles to the north. There are car parks at the feet of these mountains, a large one below Black Darren, a notable local landmark comprising a large landslip to the west of the town. There is a smaller car park below the Black Hill, and both are mainly used by walkers to access the hills. There are numerous footpaths and bridleways on the mountains, and they include Offa's Dyke Path, which runs north-south along the top of the Hatterall ridge. History Longtown has an early Norman motte and bailey ...
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Black Hill (Herefordshire)
The Black Hill (also known as ) is a hill (elevation 2100 feet or 640m) in the Black Mountains in Herefordshire, England at . It rises just west of the village of Craswall, near the border with Wales. The southern part of the ridge leading to the summit is a rocky knife-edge giving excellent views to either side. The northern part crosses a peat bog on gently sloping land at the edge of the east facing escarpment. The lower part is very similar to the main ridge of the Skirrid mountain near Abergavenny, owing to their similar underlying geology. The Black Hill is known locally as the 'Cat's Back,' as viewed from Herefordshire it looks like a crouching cat about to pounce. Access There is a very small parking (room for about 6 cars) and picnic area at the southern tip of the ridge, at the far end of minor roads leading from Longtown, Herefordshire. It is signposted at a road junction north of Longtown, and is shown on most Ordnance Survey maps of the area. The parking area lie ...
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Trig Point
A triangulation station, also known as a trigonometrical point, and sometimes informally as a trig, is a fixed surveying station, used in geodetic surveying and other surveying projects in its vicinity. The station is usually set up by a mapping organisation with known coordinates and elevation published. Numerous stations are installed on summits for purposes of visibility and prominence. A graven metal plate on the top of a pillar may provide a mounting point for a theodolite or reflector, often using some form of kinematic coupling to ensure reproducible positioning. Use Trigonometrical stations form networks of triangulation. Positions of land boundaries, roads, railways, bridges and other infrastructure can be accurately located by the network, a task essential to the construction of modern infrastructure. Apart from the known stations set up by government, some temporary trigonometrical stations are set up near construction sites for monitoring the precision and progr ...
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Gospel Pass
The Gospel Pass (Welsh language, Welsh: ''Bwlch yr Efengyl'') is the highest road pass in Wales. It is at the head of the Vale of Ewyas in the Black Mountains, Wales, Black Mountains of southeast Wales. Starting from Hay-on-Wye the narrow mountain road climbs steeply to a height of above sea level, squeezing between the mountains of Twmpa to the west and Hay Bluff to the east, before dropping down into the valley to the south on its way to Llanthony Priory, Llanfihangel Crucorney and Abergavenny. At one time a small lead-mining operation was established at the pass. The Gospel Pass is one of the most celebrated locations within the Brecon Beacons National Park, being a popular destination for sightseers and is popular too with walkers and cyclists. Indeed, the Gospel Pass road forms a part of route 42 of the National Cycle Network. It also featured in the opening scenes of the film "An American Werewolf In London". It is a single track road over most of its length, but there ...
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Hatterrall Ridge
The Hatterrall Ridge (sometimes spelled Hatterall) is a ridge in the Black Mountains forming the border between Powys and Monmouthshire in Wales and Herefordshire in England. The ridge is about long, and is followed by the Offa's Dyke Path. On the west side of the ridge is the Vale of Ewyas, and on the east side is the Olchon Valley and Black Hill. The western side of the ridge falls within the Brecon Beacons National Park. Much of the northern part of the ridge is a broad whaleback, but it narrows down considerably further south, and especially near to Llanthony Priory in the Vale of Ewyas to the west of the mountain. There is a large and prominent landslip on the eastern side of the mountain here, known as Black Darren, where a large slice of the rocks has fallen away from the main mass of the hill. The ridge to the southwest ends abruptly at the sheer cliff known as the Darren below which is a considerable landslide area extending south to the hamlet of Cwmyoy with its m ...
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Black Mountain (hill)
The Black Mountain (), is a mountain in the Black Mountains. It is the only Marilyn to fall exactly on the Welsh– English border, Powys and Herefordshire. Its parent peak, Waun Fach, lies to the west. Access The Black Mountain is the highest point on Hatterrall Ridge. Offa's Dyke Path passes along the ridge, more or less from south to north. A steeper path leads to the summit from near the former youth hostel in the Vale of Ewyas to the west. The summit is unmarked and, because of the very shallow gradients along the summit ridge, virtually impossible to determine ''in situ''. Open access to all the moorland here means that deviation from the paths is allowed. The ground is peaty and normally very wet even in good weather, especially on the highest ground. It is the highest summit in England south of Great Whernside in the Yorkshire Dales, even though higher neighbours are very close by in Wales. However, some mountain lists, such as the Nuttalls, consider the mount ...
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Offa's Dyke Path
Offa's Dyke Path () is a long-distance footpath loosely following the Wales–England border. Officially opened on 10 July 1971, by John Hunt, Baron Hunt, Lord Hunt, it is one of Britain's National Trails and draws hillwalking, walkers from throughout the world. About of the route either follows, or keeps close company with, the remnants of Offa's Dyke, an Earthworks (engineering), earthwork traditionally thought to have been constructed in the late 8th century on the orders of Offa of Mercia, King Offa of Mercia. Walking trail Traveling south to north, starting by the Severn Estuary at Sedbury, near Chepstow, and finishing at Prestatyn on the north coast, the walk will take an average walker roughly 12 days to complete. Roughly following the border in parts, and elsewhere the ancient monument of Offa's Dyke, as well as natural features such as the Hatterrall Ridge, the Dyke Path passes through a variety of landscapes. The route traces the eastern edge of the Black Mountai ...
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Calcrete
Caliche () is a soil accumulation of soluble calcium carbonate at depth, where it precipitates and binds other materials—such as gravel, sand, clay, and silt. It occurs worldwide, in aridisol and mollisol soil orders—generally in arid or semiarid regions, including in central and western Australia, in the Kalahari Desert, in the High Plains of the western United States, in the Sonoran Desert, Chihuahuan Desert and Mojave Desert of North America, and in eastern Saudi Arabia at Al-Hasa. Caliche is also known as calcrete or kankar (in India). It belongs to the duricrusts. The term is borrowed from Spanish and is originally from the Latin word , meaning lime. Caliche is generally light-colored but can range from white to light pink to reddish-brown, depending on the minerals present. Caliche is a mark of older landscapes. It generally occurs on or very near the surface. Where caliche layers originate at some depth from the soil surface, intact landscapes and buried landsca ...
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Devonian Period
The Devonian ( ) is a geologic period and system of the Paleozoic era during the Phanerozoic eon, spanning 60.3 million years from the end of the preceding Silurian period at million years ago ( Ma), to the beginning of the succeeding Carboniferous period at Ma. It is the fourth period of both the Paleozoic and the Phanerozoic. It is named after Devon, South West England, where rocks from this period were first studied. The first significant evolutionary radiation of life on land occurred during the Devonian, as free- sporing land plants (pteridophytes) began to spread across dry land, forming extensive coal forests which covered the continents. By the middle of the Devonian, several groups of vascular plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants ( pteridospermatophytes) appeared. This rapid evolution and colonization process, which had begun during the Silurian, is known as the Silurian-Devonian Terrestrial Revo ...
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