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KUL AIJAYA
SITE 7 – MENANG QUARRY,
TINGGI
SITE 8 – BJ QUARRY, KOTA
S i t e 8 – B J Q u a r r y, Ko t a T i n g g i ,
Johor.

Ju ron g Formation in Johor is the exten ded formation from Sin gapore.

Geol ogy of the stu d ied site u n d erl ain by u n p red ictab l e l ithol ogy of

a n Ol d e r a l l u v i u m a s i n Gob b e t te t a l . ( 197 3 ) . T he Ol d e r a l l u v i u m

cove rs p he n ocl a sts of ve in q u a r tz, q u a r tzite, sa n d ston e, sil tston e,

shal e, horn fel s, gran ite, gran ite porphyry, al askite, apl ite, rhyodacite,

an desite an d tu ff. The u tmost common variation is coarse fel dspatic

sa n d w ith irre g u l a r rou n d e d p he n ocl a sts, b u t g rave l y cl ay, sa n d y

Johor
g r a v e l , s a n d y c l a y , s i l t y c l a y , c l a y e y s a n d a n d c l a y a r e
Site 7 – Men an g Qu arry, Ku l ai Jaya,
presen ted
correspon din gl y

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