Indonesia

The Juru Sebrang Off-Shore Former Tin Mine

Rock and mineral: tin rich-alluvial resulted form weathering of Tanjung Pandang granite/S-type granite mixed with weathering from the metasediment of KelapaKampit Formation. Rock age origin: Permo-carboniferous and Triassic, but alluvial age is Quaternary.
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Rock and mineral: tin rich-alluvial resulted form weathering of Tanjung Pandang granite/S-type granite mixed with weathering from the metasediment of KelapaKampit Formation. Rock age origin: Permo-carboniferous and Triassic, but alluvial age is Quaternary. The Juru Seberang geosite is a tin rich-alluvial area that resulted from weathering of Tanjung Pandang granite/ S-type granite mixed with weathering from the metasediment of Kelapakampit Formation. A lamp shell (Lingula Unguis) was found in the area, the animal representing evolution from the Cambrian Period (542 million years ago)

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