...R. L. Ethington Synopsis Conodonts in a sample collected from the Margie Limestone in an abandoned quarry along the bank of the River North Esk near Edzell include elements of the apparatuses of Paracordylodus gracilis Lindström and of a species tentatively reported herein as Prioniodus sp...

...Fig. 4. ( A ) Outline geological map of the River North Esk section NW of Edzell, and the location of samples NE11A, 129–134. The position of the Highland Boundary Fault is obscured by the outcrop of the Lintrathen Porphyry (not shown). ( B ) Simplified geological map of the HBC in North Glen...

...Donald M. Ramsay Abstract The fracture pattern of pebbles in lower Old Red Sandstone conglomerates of various localities between Loch Lomond and the North Esk river, Scotland, indicates that the southern component of the principal compression along the Highland Boundary fault was a continuation...

... Linn with river North Esk’, which indicates locality R82 along the river North Esk, about 100 m north of the confluence with the Wether Law Linn. The specimen is an internal mould of a dorsal valve. This specimen is registered as number NMS G.2016.4.1. Description. Dorsal valve flat, transverse...

... Highland Group–Trossachs Group transition in the Loch Ard Forest. ( c ) A472. (Meta-)feldspathic arenite, Lower Keltie Water Formation in Leny Quarry, Callander. ( d ) NE148. (Meta-)calc-quartz arenite, from adjacent to the Margie Limestone in the River North Esk section. ...

... ) for the River Irt, and 4.2 m 3 s −1 (13.78 ft 3 s −1 ) for the River Esk ( Bousher, 1999 ). Anthropogenic impact on the estuary is here considered to be minor, excluding the sheltering of the inner Mite from tidal currents and increased salt marsh development as a consequence of the railway viaduct...

... this height a magnificent panorama unfolded below us of the terraced valley of the North Esk River. There seemed to be many small exposures along its banks. Opposite us the ravine of Wether Law Linn extended away and upwards from its confluence with the main river, and here too were fine exposures, which...

... Bridge Sandstone Formation. ATi–apatite–tourmaline; CZi – Chrome-spinel–zircon; GZi – garnet–zircon; MZi – monazite–zircon; RuZi – rutile–zircon. This formation is more or less continuously exposed along the River Esk in the immediate area north and south of Canonbie Bridge ( Fig. 2 ) and its base...

... of the lapworthi Biozone. Fig. 1. Biostratigraphically significant graptolites from the Deerhope Formation, North Esk Inlier. ( A ) BGS 17E 7045, Oktavites of the spiralis group, distal fragment, Deerhope Coral Bed at NT 1455 5802. ( B ) BGS EMI 183, Diversograptus ramosus Manck 1923 , lower...

...S. G. Molyneux; H. F. Barron; R. A. Smith Synopsis The results of a palynological study on late Llandovery–Wenlock (mid-Silurian) successions in the North Esk, Bavelaw Castle and Loganlee inliers of the Pentland Hills, Midland Valley of Scotland, are documented. Palynological assemblages from...

... Formation, North Esk River, first exposure above Wether Law Linn. TCD 51010, (R101), upper Wether Law Linn Formation, large exposure on southern bank of North Esk River above junction with Henshaw Burn. NMS G 2000.41.1, Deerhope Burn. TCD 51015, TCD 51016, (R245), Deerhope Formation, Deerhope Burn. 16...

... Cret Cape Palliser, lighthouse access S28/008525 2 17B MUKA1 24303 Kaweka Terrane Esk Head Belt Late Jurassic Mukamuka Stream, Palliser Bay R28/797786 5 Marlborough – North Canterbury 18 LTHM1 23060 Kaweka Terrane Esk Head Belt Late Jur – Early Cret Leatham River Valley...

... clasts, mainly comprising fine foliated or schistose low-grade metapelitic and metapsammitic fragments. The formation is well exposed along the River Esk between ~ 250 m south and ~ 600 m north of Canonbie Bridge ( Fig. 2 ). Borehole records show that the formation ranges in thickness from 131 to 168 m...

.... The possibility that the source rocks for these sequences are within the Midland Valley Terrane, but now not exposed, is discussed. Minor differences in sandstone composition between the Carmichael, Eastfield and North Esk inliers are interpreted as reflecting either slight differences in the source or deposition...

... Border series to the SE, for c . 2 km. At one location a lens of the 'Margie Series' is isoclinally folded. The North Esk river exposes one of the best inland sections of the complex which was described by Johnson & Harris (1967) . There is a sequence of black shales, pillow lavas, agglomerates...