(2) Lokasi Saluran Penghantar (Wate

(2) Lokasi Saluran Penghantar (Waterway)
Batuan pondasi pada Saluran Penghantar (Waterway) sebagian besar merupakan satuan batuan yang merupakan perselingan antara serpih, napal dan batupasir gampingan yang pada permukaannya sudah mengalami pelapukan sedalam 2-4 m dan dibeberapa tempat oleh endapan longsoran, hanya pada bagian tengah lebih kurang 500 m merupakan endapan longsoran dari breksi volkanik yang berada diatasnya, terdiri dari bongkah – bongkah andesit keras diantara tanah pelapukan lempungan yang lunak.

結果 (英文) 1:

(2) Location of conducting Channels (Waterway)
Rock Foundation in Conducting Channel (Waterway) is largely a rock unit that is perselingan between the shale, marl sandstones and its current state, which on the surface has been subjected to weathering as deep as 2-4 m long and in some places by Avalanche deposits, only in the Middle, more or less 500 m is the deposition of the breksi volcanic avalanches that are on top of it, consists of the bongkah – bongkah hard andesite among soil weathering soft lempungan.

結果 (英文) 2:

(2) Location dissipation channel (Waterway)
rock foundation on Channel dissipation (Waterway) is largely a lithologies is perselingan between shale, marl and calcareous sandstone which has experienced weathering surface 2-4 m deep and in some places by sediment avalanches, only the central part of approximately 500 m was precipitated avalanches of volcanic breccia which is above, is composed of chunks - chunks of hard andesite between weathering silty soft soil.