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Svallarp Destination Guide
Explore Svallarp in Sweden
Svallarp in the region of Jönköping is a town in Sweden - some 160 mi or ( 257 km ) South-West of Stockholm , the country's capital city .
Current time in Svallarp is now 11:48 PM (Saturday) . The local timezone is named " Europe/Stockholm " with a UTC offset of 1 hours. Depending on the availability of means of transportation, these more prominent locations might be interesting for you: Copenhagen, Växjö, Stora Okna, Stockholm, and Sjunnen. Since you are here already, make sure to check out Copenhagen . We encountered some video on the web . Scroll down to see the most favourite one or select the video collection in the navigation. Where to go and what to see in Svallarp ? We have collected some references on our attractions page.
Videos
Goldsuche in Schweden
Goldsuche in Schweden in Ädelfors bei Vetlanda ..
Guldvaskning Ädelfors i Vinterdvala
Guldvaskning i Ädelfors i Vinterdvala. Emåns isiga vattnet rinner stilla o ostörd. *** Goldwaschen in Ädelfors hält Winterschlaf. Das eisige Wasser des Emåns fliesst still und ungestört. © by romywebb ..
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 ..
Vattnet forsar i Sjunnen
Vattnet forsar i Sjunnen . Stromschnelle in Sjunnen © 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 12 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 24 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.