カーマーゼンシャーの絶景の山頂・トップ14

https://hoofhike.com/ 👈

https://hoofhike.com/

Moderate trail for all to explore and enjoy the beautiful sceneries

Garreg Las (Twyn-Swnd) is on the west side of the Black Mountain range, and it is visited far less often than many peaks in the Brecon Beacons. Its remoteness is its draw for me; rarely will you be unindated with a host of other walkers here. It is also hansomely topped by a pair of substansive, rocky ancient cairns. You can come across from the car park on the A4069 Brynaman Road or come up from Llanddeusant; both are equally as appealing, but the Llanddeusant route takes the top slot if you go back via Llyn y Fan Fach; this route has the best views. The views from the summit itself are like the location: raw and remote, but I love the place. It is a good area for a bit of navigation practice. At 635 metres high, it is a UK-listed Nuttall and Hewitt. Tip: Any Welsh place name with Llan in it means it has a church. In this case, Llanddeusant means the church with two saints.

At just 440 metres Tair Carn Isaf is a modestly sized hill, but its prominence at the western end of the Black Mountain, high above the Amman Valley, affords extensive views over central south Wales, into Powys, west to the Preselis, and over the Gower Peninsula and Severn Estuary.

Garreg Lwyd, also known as Moel Gornach, is a peak in the Black Mountain of the Brecon Beacons, South Wales. It is a subsidiary summit of Fan Brycheiniog. It is the westernmost area over 2,000 feet above sea level in South Wales.

ここは、ウェールズ西部にあるブレコン・ビーコンズの非常に過小評価されているエリアです。ここのハイキングは荒々しくワイルドで、公園の中でも静かなエリアである理由の一つであり、多くの人にアピールするでしょう。また、ここには、これまで見た中で最高の鉄器時代の丘砦の例がいくつかあります。 Y Garn GochとY Gaer Fachは、ウェールズで最も印象的な丘砦のいくつかです。それぞれ11.2ヘクタールと1.5ヘクタールで、これらは印象的な構造物であり、当時、先住民にかなりの防御構造を提供していました。大きな石の防御壁は、今日では大きな瓦礫の土手ですが、かつては高さ10メートル、厚さ5メートルでした。両方の砦には、丘のふもとにある小さな駐車場からアクセスできます。

Picws Du is the second highest peak of the Carmarthen Fans in the Carmarthenshire section of the Black Mountain in the west of the Brecon Beacons National Park in south Wales.Picws Du is formed from the sandstones and mudstones of the Brownstones Formation of the Old Red Sandstone laid down during the Devonian period. Its summit and southern slopes are formed from the hard-wearing sandstones of the overlying Plateau Beds Formation which are of upper/late Devonian age.