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Rhiconich Destination Guide
Delve into Rhiconich in United Kingdom
Rhiconich in the region of Scotland is located in United Kingdom - some 515 mi or ( 829 km ) North of London , the country's capital .
Local time in Rhiconich is now 11:48 AM (Saturday) . The local timezone is named " Europe/London " with a UTC offset of 0 hours. Depending on your mobility, these larger destinations might be interesting for you: Stornoway, Newcastle-on-Tyne, Kylestrome, Inverness, and Glasgow. While being here, you might want to check out Stornoway . Are you curious about the possible sightseeing spots and facts in Rhiconich ? We have collected some references on our attractions page.
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Interesting facts about this location
Easan Garbh
Easan Garbh is a waterfall of Scotland.
Located at 58.43 -4.97 (Lat./Long.); Less than 1 km away
Eas na Glutachan
Eas na Glutachan is a waterfall of Scotland.
Located at 58.45 -4.95 (Lat./Long.); Less than 4 km away
Kinlochbervie High School
Kinlochbervie High School (Scottish Gaelic: Ard Sgoil Cheann Loch Biorbhaidh) is a secondary school in Kinlochbervie, in the county of Sutherland in the northwest of Scotland. The school is attended by around 65 pupils from a catchment area that extends from Scourie to Durness. Before the school opened in 1995, pupils attended Golspie High School as weekly boarders.
Located at 58.46 -5.03 (Lat./Long.); Less than 5 km away
Foinaven
Foinaven is a mountain in Scotland, situated in the far north-west corner of the Scottish Highlands. Like many of the monolithic mountains that surround it, the mountain is within the Moine Thrust Belt and is made up of imbricated layers of Cambrian quartzite which overlie the older Lewisian gneiss basement. The quartzite, being tougher, stood firm when all the surrounding rock was eroded away, leaving the huge mountain isolated. Its highest point is named Ganu Mòr.
Located at 58.41 -4.89 (Lat./Long.); Less than 6 km away
Arkle (Sutherland)
Arkle is a mountain in Sutherland, situated in the far north-west corner of the Scottish Highlands. Like its sister Foinaven, the mountain is made up of glistening white Cambrian quartzite, laid down around 530 million years ago on an uneven basement of much older Lewisian gneiss.
Located at 58.37 -4.90 (Lat./Long.); Less than 8 km away
Related Locations
Information of geographic nature is based on public data provided by geonames.org, CIA world facts book, Unesco, DBpedia and wikipedia. Weather is based on NOAA GFS.