Rafting at Palayangan River who have unique variations of rapids:
1. Drop, formed due to a decrease in the riverbed such as The Shape of a ladder / step down on the riverbed but not too big (like a small waterfall). This type can be found in the rapids of sheep I and sheep II.
2. Double Drop, formed due to river currents passing through or over large rocks. It is called a double drop because of The Shape of the current, which resembles a successive waterfall. This type can be found in Rapids Kacapi.
3. Turbulence, is a wave swirling below the surface of the water that is usually formed due to the depth of the river decorated with large rocks or the fall of water from a previous height. This type can be found in Welcome Rapids & Blender Rapids.
Pangalengan, Bandung, Indonesia
Across Situ Cileunca by traditional boat from meeting point to Seribu Pulau Pangalengan
1. Drop, formed due to a decrease in the riverbed such as The Shape of a ladder / step down on the riverbed but not too big (like a small waterfall). This type can be found in the rapids of sheep I and sheep II. 2. Double Drop, formed due to river currents passing through or over large rocks. It is called a double drop because of The Shape of the current, which resembles a successive waterfall. This type can be found in Rapids Kacapi. 3. Turbulence, is a wave swirling below the surface of the water that is usually formed due to the depth of the river decorated with large rocks or the fall of water from a previous height. This type can be found in Welcome Rapids & Blender Rapids.
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