. Memoirs of the Geological Survey of India . sj*>> Ti£. 33. Vvrest ci Saj. Fit, 34. ? ast 01 Saya NUMMULITIC ELLIPSOID FROM MANZULLI TO BANDa. 137 structure of the ground, as shown in the sections, Figs. 32, 33, and 34,of the Saya ellipsoid, (Malgin salt quarries) about one mile in extent,each. 1. Rock-salt. 2. Gypseous series. 3. Red clay zone. 4. Numraulitic limestone. 6. Tertiarysandstones. F. Faults. The salt of this locality will be found referred to in the appendix ; it is of the usual dark gray colour, and like thatRock-salt. . of other eastern localities, the upper part is mplac
. Memoirs of the Geological Survey of India . sj*>> Ti£. 33. Vvrest ci Saj. Fit, 34. ? ast 01 Saya NUMMULITIC ELLIPSOID FROM MANZULLI TO BANDa. 137 structure of the ground, as shown in the sections, Figs. 32, 33, and 34,of the Saya ellipsoid, (Malgin salt quarries) about one mile in extent,each. 1. Rock-salt. 2. Gypseous series. 3. Red clay zone. 4. Numraulitic limestone. 6. Tertiarysandstones. F. Faults. The salt of this locality will be found referred to in the appendix ; it is of the usual dark gray colour, and like thatRock-salt. . of other eastern localities, the upper part is mplaces somewhat bituminous near where it is in contact with the over-lying black bituminous gypseous rock; from the situation of the quar-ries its thickness may be over 200 feet. There is a rather large accumulation of boulders and debris along the foot of the hill west of Saya, now at a higherBoulder accumulation. level than that at which the river runs, but which may nevertheless have been brought together by the transporting agency of this Teeree Towey (Tiri Taui) stream in
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