Llangenny

Cwrt-y-Gollen ("Hazel Court") is a British Army training base, 2 miles (3 km) south-east of Crickhowell and just north of the A40 road and the River Usk, in southeastern Powys, Wales.

Glangrwyney or Glangrwyne is a village 2 miles (3.2 km) southeast of Crickhowell in Powys, Wales. The village is where the Grwyne Fawr has its confluence with the River Usk, southeast of the Sugar Loaf and at the junction of the road from Gilwern with the A40 trunk road. Glangrwyney is in the Vale of Grwyney Community for administrative purposes. The village is built upon the sands and gravels of a dissected alluvial fan which extends into the floodplain of the Usk, together with till derived from the former Usk Valley glacier.Facilities in the village include a village hall and The Bell public house. The former army training camp of Cwrt y Gollen is on the western edge of the village.

Llanbedr is a small village 2 miles (3 km) northeast of Crickhowell in the county of Powys, Wales and the community of Vale of Grwyney. It lies above the river known as the Grwyne Fechan just above its confluence with the Grwyne Fawr in the southern reaches of the Black Mountains range. The village lies within the shadow of Table Mountain, an outlying spur of Pen Cerrig-calch on which is perched the Iron Age hill fort of Crug Hywel.The church of St Peter is a grade II* listed building.

The Grwyne Fawr is a river in the Brecon Beacons National Park in south Wales. A section of it forms the administrative border between Powys and Monmouthshire and also of the historic counties of Brecon and Monmouth. The river and its major tributary the Grwyne Fechan flow into the River Usk at Glangrwyney.The name probably originates from gweryn or gwerynau and mawr/fawr meaning 'large river at the wet place'. The Gwryne Fawr rises at Blaen Grwyne Fawr on the southern slopes of Rhos Dirion in the Black Mountains and follows a southeastward course for several miles, its flow interrupted by the presence of Grwyne Fawr Reservoir, the only waterbody within this range of hills. Some way below the reservoir, Mynydd Du Forest clothes the sides of the valley. Though a public road penetrates the valley as far as the north end of the forest, the valley is very sparsely populated. It is only approaching the hamlet of Partrishow that the valley takes on a farmed appearance. The river now heads west along a valley whose alignment is guided by the presence of a geological line of weakness known as the Neath Disturbance. To the west, the Grwyne Fechan takes a parallel course to that of its larger neighbour. It rises on the southern slopes of Waun Fach and gathers a number of tributary streams from the broad ridge which separates it from the Grwyne Fawr. Though there are numerous conifer plantations, the valley has a more open aspect than that of the Grwyne Fawr. The two rivers join near the village of Llanbedr and head south as the Grwyne Fawr through the hamlet of Llangenny to their confluence with the River Usk at Glangrwyney.

Y Graig, three miles west of Abergavenny, is the site of an abandoned settlement, known to have been occupied in the 18th and 19th centuries. It is a scheduled monument in the care of Cadw.

The Church of St Elli, Llanelly, Monmouthshire, Wales, is a parish church with its origins in the 14th century. The church underwent three major restorations, in 1867–1868, 1897 and 1910–1911. It remains an active parish church and is a Grade II* listed building. The church is dedicated to the 6th-century Saint Elli, who may have been a daughter or granddaughter of King Brychan, or a male disciple of Saint Cadoc.

Crickhowell Castle (Welsh: Castell Crucywel) is a Grade I listed building in Crickhowell, Wales, now largely ruined. An alternative name, "Alisby's Castle", is sometimes used; this is thought to be after a former governor of the castle, Gerald Alisby.

Llanelly (Welsh: Llanelli) is the name of a parish and coterminous community in the principal area of Monmouthshire, within the historic boundaries of Brecknockshire, south-east Wales. It roughly covers the area of the Clydach Gorge. The population of the parish and ward at the 2011 census was 3,899.

Crug Hywel is an Iron Age Celtic hillfort, with a clearly visible earth and stone ditch and rampart. Crug Hywel is approached by a couple of public footpaths across farmland from Crickhowell and Llanbedr and visited by the Beacons Way. It lies within an area designated as open country over which the public have the right to roam. The name is sometimes given to the flat-topped hill itself, which is also called Table Mountain in English. Located at the southern edge of the Black Mountains in south-east Wales, it rises to 451 m above sea level, from the southern flank of Pen Cerrig-calch (701 m), and overlooks the town of Crickhowell, whose name derives from Crug Hywel.The Welsh name Mynydd y Begwn is also used for this summit. As a result, it has been suggested that the name Crug Hywel (which means 'Hywel's mound') may originally have referred to the castle mound in Crickhowell.

The Bear Hotel, formerly the White Bear, stands on Beaufort Street, Crickhowell, Powys, Wales. A coaching inn from the mid 18th century, the building has older origins from the 17th and 15th centuries. It is a Grade II* listed building.

Crickhowell (; Welsh: Crucywel pronounced [krɨkːəu̯ɛl], non-standard spelling Crughywel) is a town and community in southeastern Powys, Wales, near Abergavenny, and is in the historic county of Brecknockshire.

Crickhowell Market Hall (Welsh: Neuadd y Farchnad Crucywel), formerly Crickhowell Town Hall (Welsh: Neuadd y Dref Crucywel), is a municipal building in the High Street, Crickhowell, Powys, Wales. The structure, which accommodates market stalls on the ground floor and a café on the first floor, is a Grade II* listed building.