794 JOURNAL, BOMBAY NATURAL HIST. SOCIETY, Vol. XXIII. 



line 30 miles North of the second, forming the "islands" of Putchum, 

 Kareer, &c., in the Runn. The first line I have sketched as it occurs at 

 Ler, Fakirwadi, Bharasar and Sumatra. The second line has been illustrated 

 by its exposure at Keera Hill, to which I now add the exposure in the 

 Habye Hills. The third line must wait a bit. 



Sequence op Ouxch Ammonite beds. 



The inset table shows the 

 sequence of the Ammonite 

 beds in Cutch. The " Sub- 

 Anceps beds " are an ad- 

 dition of my own to the 

 usually recognized list ; for 

 there seems to me to be a 

 distinct type of rock coming 

 up from below the Anceps 

 in which I have found no 

 Anceps fossils : yet it lies 

 much above the Macroce- 

 phalus beds. A fossil much 

 like Waagen's Peris2)Ji, Per- 

 dagatus seems its charac- 

 teristic. 



Oomia beds (Neocomian). 

 Ketrol beds (Kimekidge). 

 Dhosa Oolite (Oxfokdian). 

 Athleta beds (Oallovian). 

 Anceps beds (Callovian). 

 Sub-Anceps (Callovian). 

 Macrocephalus beds (Callovian). 

 Putchum beds (Bath). 



HABYE 



HILLS. 



"^^ZZZZZZZZZZZZZZZZZZZZZZZ 



KHA5 HILLS 



North-East of Bhuj, some 12 to 15 miles away, rise the Habye Hills, a 

 chain 9 miles long and two miles wide, tapering somewhat suddenly at 

 both ends before diving down again below the level of the plain. Their 

 highest points are about 800 feet high. To explore them the village 

 of Habye, once the site of Cutch's capital, makes a good he ad-, quarters. 

 It lies on the south side of the hills, 2|- miles from their east end. As 

 you approach the hills from Bhuj, you cross the ridge of the Khas hills 

 which consist of cold yellow and brown sandstone slabs, guiltless of 

 Ammonites. They dip south and are scarped on the north front ; probably 

 at one time they extended further north and formed a sheet covering the 

 whole of the Habye Hills. Climbing down the scarp, you find yourself in 

 a flat valley some two miles wide stretching up to the base of the Habye 



