Svoboda | Graniru | BBC Russia | Golosameriki | Facebook

To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

From Wikipedia, the free encyclopedia

Fan Frynych
Fan Frynych from the summit of Craig Cerrig-gleisiad
Highest point
Elevation629 m (2,064 ft)
Prominence74 m (243 ft)
Parent peakFan Fawr
ListingHewitt, Nuttall
Naming
Language of nameWelsh
Geography
LocationPowys, United Kingdom
Parent rangeBrecon Beacons
OS gridSN969193
Topo mapOS Landranger 160

Fan Frynych is the northernmost peak of the Fforest Fawr massif in the Brecon Beacons National Park, South Wales. It is classed as a subsidiary summit of Fan Fawr and makes up half of the Craig Cerrig-gleisiad and Fan Frynych National Nature Reserve with its sister peak Craig Cerrig-gleisiad.

The summit is marked by a trig point, where the northern face of Craig Cerrig-gleisiad can be viewed.[1]

YouTube Encyclopedic

  • 1/3
    Views:
    321
    1 298
    2 594
  • Fan Fawr & Craig Cerrig-gleisiad. 06/03/2010
  • Brecon Beacons - Mountain Hiking
  • BRECON BEACONS NIGHT TREK - Not A Bushty Walk In The Woods

Transcription

Geology

The upper parts of the mountain are formed from brown-coloured sandstones of the Senni Formation. At lower level and hence older, and forming the lower northern slopes, though largely unseen, are the mudstones of the St Maughans Formation. Both are units of the Lower Old Red Sandstone of early Devonian age. Though locally variable, the rock strata dip generally towards the southeast. The northeastern flank of the mountain is defined by a NE-SW aligned geological fault, the Cribarth Fault downthrowing to the southeast, which forms a part of the Swansea Valley Disturbance. Large parts of the mountain's eastern flanks are affected by landslips.[2][3]

Access

Being 'mountain' and/or 'moor', the entire mountain is mapped as open country and hence freely available to walkers under the access provisions of the CROW Act 2000. A network of paths and tracks cross its summit plateau and link with public rights of way to east, west and north. The 99 mile Beacons Way passes over Craig Cerrig-gleisiad immediately to its south, affording views over Fan Frynych's southern slopes and connecting with a path running the length of the east side of the plateau.[4]

References

  1. ^ Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. ISBN 1-85284-304-7.
  2. ^ "GeoIndex - British Geological Survey". mapapps2.bgs.ac.uk. Retrieved 30 July 2021.
  3. ^ Pillay <[email protected]>, Ruven. "IIPMooViewer 2.0: HTML5 High Resolution Image Viewer". iipimage.sourceforge.net. Retrieved 30 July 2021.
  4. ^ "Maps". www.bing.com. Retrieved 30 July 2021.

External links

51°51′49″N 3°29′56″W / 51.8635°N 3.4988°W / 51.8635; -3.4988


This page was last edited on 16 July 2023, at 18:35
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.