Memoir of the Economic Geology of Navanagar State in the Province of Kathiawar India

ppean e 32 History of 014.; Formation of the Barda and Alech groups of Hills 3 Hypabyssal Rocks of the Barda group of Hills. 33 Scenery due to Jointing and Weathering of the Hypabyssal Rocks of.the Barda and_Alech Hills The term Felsite ' restricted to Rocks of Hypabyssal Origin. Hypabyssal Rocks of the Alech group of IIills. Granophyric Rocks of the Alech Hills. Felsitic Rocks of the Alech [...] 52-53 PLATE VIii.—Photomicrographs of OLIVINE-DOLERITE Central Part of Dyke 4 Mile E. of Kandorna ; and the BASALTOID CONDITION OF THE SAME ROCK from the Edge of the Dyke. 56-57 PLATE IX.—Photomicrographs of TYPICAL COMPACT BASALT OF BEDDELAVA Summit of Hog-backed' Hill Surda to show Occasional Phenocrysts of Felspar and of the SAME RocK to show Occasional Phenocryst of Augite 6o-61 PL [...] 983 Allowing for sundry sinuosities the sea-coast of the State of Navanagar in the Gulf of Kutch taken from the mouth of Hanstal Creek (leading into the Little Ran of Kutch) to a point midway in the small ran which divides Western Extent of the Seacoast in Navanagar from the Okhamandal Tthe State of Navanagar. [...] Vinu the loftiest summit of the Barda group of hills in soutwestern Navânagar attains the height of 2057 feet above the selevel ; but the rocks in this locality are probably all of hypabyssal origin of the nature of granophyric Hypabyssal character of the felsites granophyres and kindred terocks forming the Barda Hills in the State of Navanagar. [...] Immediately east of the Barda group the State of Navanagar claims a fair half share of the complicated congeries of elevations known as the Alech Hills the members of which rise to elevations of from 396 to as much as 745 feet Complicated character of the above the level of the sea.