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Branthalla Destination Guide
Discover Branthalla in Sweden
Branthalla in the region of Jönköping is a place located in Sweden - some 158 mi or ( 254 km ) South-West of Stockholm , the country's capital .
Local time in Branthalla is now 08:22 AM (Thursday) . The local timezone is named " Europe/Stockholm " with a UTC offset of 1 hours. Depending on your mobility, these larger cities might be interesting for you: Copenhagen, Växjö, Stora Okna, Stockholm, and Skinnberga. When in this area, you might want to check out Copenhagen . We discovered some clip posted online . Scroll down to see the most favourite one or select the video collection in the navigation. Are you looking for some initial hints on what might be interesting in Branthalla ? We have collected some references on our attractions page.
Videos
Holsby Kvarn i Holsbybrunn
Holsby Kvarn i Holsbybrunn med sitt brusande vatten från Emån. *** Die Holsby Mühle in Holsbybrunn mit ihrem vom Emån kommenden brausenden Wasser © by romywebb.se ..
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Interesting facts about this location
Ädelfors folkhögskola
Ädelfors Folkhögskola (Ädelfors folk high school) is a Swedish folk high school which is specialized in teaching disabled people and people with special needs. The school is located in Holsbybrunn in Vetlanda. It offers courses in a variety of subjects, and its students come from all over the country.
Located at 57.44 15.20 (Lat./Long.); Less than 15 km away
Skuruhatt
Skuruhatt is a steep hilltop near Skurugata in Eksjö Municipality with a great view of the hinterlands of Småland in southern Sweden. Nearby a stone has been placed with the following Swedish inscription by Albert Engström. Folket som bor i dessa gårdar torde vara av renaste guld -- dessa sega magra arbetare som brottas med sin fattiga jord och segra, segra är det icke ett folk att hålla av. Albert Engström
Located at 57.70 15.08 (Lat./Long.); Less than 19 km away
Skurugata
Skurugata is a rock canyon in southern Sweden, an 800 metre long gorge which runs 20 to 50 metres deep and 7 to 24 metres wide. There are several different theories for its origin but one of the more popular theories is that it was created by parallel faulting. The mountain around the gorge itself and the stones spread across its bottom consist largely of grey-brown and dark-brown porphyritic rock with elements of quartz and red feldspar.
Located at 57.71 15.09 (Lat./Long.); Less than 20 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.