Tuesday, October 18, 2016


Cold Spring




TUBOD  


It is located in Lanoy,Jagna, Bohol. It is just around 15-30 minutes of travel from the town's proper. 
Tubod is a cold spring where you can take a bath, drink fresh water, even wash your clothes and find (soso) shell for food.






badiang spring



Badiang Spring in Valencia is 44 km from Tagbilaran City. An underground freshwater spring gushes from twin pipes near the sea. The springwater is diverted to fill 2 swimming pools, one large and the other for children. Sheltered picnic tables are on a veranda overlooking a smooth-stone beach.
Badiang Spring is an underground freshwater spring that gushes forth over a cliff only a few meters high forming an attractive waterfall. The water is icy cold and flows directly to the sea which is only a few steps away.




CANAWA SPRING



The Can-umantad Trail trek starts at Canawa Spring in Barangay Can-umantad. The Canawa Spring is another natural wonder; a spring with an underground source since no water source feeds it from the outside. Trekkers can stop and enjoy a short dip in the pool of the bluest blue before proceeding further inland.






TIGDAO SPRING





Tigdao Spring/Cave can be found in Anda town. A karst limestone cavern holds fresh spring water which is only a few inches from the rim. Spelunkers have explored the inner recesses of the cave and found no major tunnels. Tigdao Spring looks like a big natural well.






BANILAD SPRING





Banilad Spring/Cave also in Anda was once a major religious pilgrimage site. The cave is situated near some ruins which are almost covered by vegetation. Stone steps lead to the cave opening. Inside is a cavern with a tunnel that appears very constricted.












KALORENZO SPRING



Kalorenzo Spring/Cave in Anda is a typical karst cave with a wide opening and a spring water pool below it. The cavern inside is wide and spacious with typical formation of stalactites and stalagmites with the water up to the chest only. A tunnel which is only a few meters long can be found inside. Further entry to the tunnel is restricted due to localized constriction fringed by unstable-looking karst formation.

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