... of the Frasnian, notably in the Kakisa Formation of southern District of Mackenzie and northeastern British Columbia, the Simla and uppermost Mount Hawk formations of the Rocky Mountains and Blue Ridge Member of the Alberta subsurface. Species with a com- parable range include Chuanbeiphyllum vesieulosum, C...

... are indicated. Key to lithostratigraphy: F—Flume Formation, C—Cairn Formation, Pe—Peechee Member, A—Arcs Member, S—Simla Member, R—Ronde Member, M—Maligne Formation, P—Perdrix Formation, H—Mount Hawk Formation. Key to stratigraphic sections: MC—Marmot Crack, A/C—Thornton Creek, AB and W4—Poachers Creek, KC...

... position of the Nahans (Lower Siwaliks) in the Tertiaries of north-western Himalayas (Table I) has ever remained an enigma mainly because of their close apparent lithological resemblance with the underlying Dagshai/ Kasauli sequence. Though the Nahans of the Simla Hills have been studied in their various...

... of the minerals, 'signs of dynamo-metamorphism are some- times displayed, and pink garnets almost invariably appear'. Holland (1900, p. 141) did not notice garnet in the unaltered type mass near St. Thomas Mount but reports that this mineral is an invariable constituent of the Hevarieties which have suffered from...

... the structural and metamorphic history of the Simla Klippe and raises the question of the inverted metamorphic zoning within the Jutogh series, a problem which, however, concerns a much more extensive area in the Himalaya than just around Simla. Pilgrim a.1d West (1928) were the first to consider the possibility...

... Bistro (211 ft .) , Thornton Creek (200 ft Mount Simla (234 ft Fiddle River canyon (20 6 ft and Solomon Creek (145 ft .) (see Walasko, Lerbekmo and Mountjoy , Fig. 1, 1964. These variations in thickness are likely due to a number of factors ; irregularities on the sea floor, differences in amount of lime...

... way back home. I invited him for a lunch and showed my paintings and particularly the one of Mount Kailas, based on his photograph, he seemed to like it. After lunch we started discussing Ladakh geology. I showed my Zanskar map sheets and also the geological maps of Simla area and Ladakh. He wondered...

... of the Simla and Baliana Rivers (Lat. 31°1ʹ1.4ʺN, Long.77°0ʹ26.0ʺE) the diamictite is found resting directly on light brown shale ( Fig. 3A ). On the Yashwant Nagar–Rajgarh Road section (Lat. 30°53ʹ13.38ʺN, Long. 77°14ʹ13.32ʺE) the diamictite is found to rest on a fault scarp above the older rocks of Simla...

... and an unnamed lower member . Field work in 1968 by Mountjoy clearly showed that the base of the Simla Member in Mount Haultain cirque does not end ab- ruptly as previously thought, but the member passes southeastward into a thin tongue of the upper part of the Mount Hawk Formation . Mountjoy and MacKenzie...

... southwest of Simla presented here indicate that total slip occurred 190 km along strike. We reconcile the apparent discrepancy in these two new constraints by noting that the slip quantified by the geodetic data includes a time period during which a large aftershock occurred ≈ 120    km...

...) and the Krummedal sequence (Higgins, 1976), an older group or perhaps the migmatised equivalent of the Eleonore Bay Group, compare in thickness and regional significance with Himalayan Proterozoic sediments such as the Simla Group and Shali Formation in Himachal Pradesh (Bhargava, 1972). Fundamental problems...

... controlled hydrothermal uranium mineralisation in the Central Gneissic Complex at Chaura, Simla district, H.P. and overlying crystalline nappe rocks as at Brijranigarh (Tehri district, Uttrakhand) and Kasha (Simla district, HP) (b) Syngenetic type uranium mineralisation at Kanum (Kinnaur, HP) in Carbonaceous...

..., 1973 , modified after Acharyya and Shah, 1974 ). Early Paleozoic Jaunsar and Simla Groups are similar in lithologic organization but latter usually are free of bedded volcanic rocks. Porphyritic pre-Tertiary granite is present ( Srikantia and Bhargava, 1974 ). Several late Paleozoic-Triassic (393, 228...

... platforms is represented by the Ronde and Simla Members of the Southesk Formation, respectively, whereas coeval strata of the uppermost Mount Hawk Formation comprise equivalent slope and basin facies. Facies of the Lower Ronde and Simla and uppermost Mount Hawk Formation include carbonate-poor argillaceous...

... A. Gansser A. Central Himalaya. Geological observations of the Swiss expedition 1936 Denkschr. Schweiz. naturf. Ges. 1939 73 245 Heron A. M. Geological results of the Mount Everest reconnaissance Rec. geol. Surv. India. 1922 54 215 34 Holland C. H. A guide...

... by the present writer. Further investigation of the organic matter in this and other Australian Tertiary oil shales ( Figure 1 ), using both strew mounts and fluorescence-mode examination of polished surfaces parallel with bedding, has shown that most of the organic matter is derived from planktonic algae...

... role in the subsequent localization of the Southesk-Cairn platform margin in the Mount MacKenzie area during Cairn time. The Cairn margin has a transgressive, wedge-shaped profile. It is primarily composed of skeletal grainstones and represents a ramp-style bank-to-basin transition. The Cairn platform...

..., but no damage was reported. Simla, India, October 20, 1937A severe earthquake at 6:45 A.M. toppled over chimneys and caused roofs to collapse on houses over a wide area. The shock was felt as far away as Delhi, where doors and windows rattled. Imperial, California, October 21, 1937A slight earthquake was felt...

...), Mohand Rao (6), Chillawala Rao (7), Gaj Rao (8), Binj Rao (9), Harnaul Sot (10), RaoIi Turkee Kalakund (11) and Ranipur Hardwar Bagh Rao (12). Krynine (1937) did not notice any distinct change in the heavy mineral residues of the Siwaliks exposed in the'near vicinity of Rawalpindi (Pakistan) and Simla...