960 THE GEOLOGY OF SOUTH-EASTERN KINCARDINESHIRE. 
1912. Jenu, T. J., “ Discovery of Fossils in the Chert and Black Shale Series at Aberfoyle,” Nature, vol. 
Ixxxix. p. 347, and Geol. Mag., dec. 5, vol. ix. p. 469. 
1912. Prac, B. N., The Relation between the Cambrian Faunas of Scotland and North America, Presidential 
Address to Section C, British Association. © ; 
1912. Traguar, R. H., “Note on the Fish-remains collected by Messrs R. Campbell, W. T. Gordon, and 
B. N. Peach in Paleozoic Strata at Cowie, Stonehaven,” Geol. Mag., dec. 5, vol. ix. p. 511. 
XVIII. EXPLANATION OF PLATES. 
Prate I. 
Fig. 1. Ruthery Head, near Stonehaven. The white line indicates the position of the unconformable 
junction between the Upper Cambrian (C) and Downtonian (D). | 
Fig. 2. Ruthery Head. Nearer view of another part of the Tagen aie) junction shown in fig. 1. 
The broken white line marks the position of a small fault. 
Fig. 3. Craigeven Bay, Stonehaven. Downtonian rocks in the foreground ; Upper Cambrian strata of 
Garron Point on the far side of the bay. 
Fig. 4. Coarse conglomerate resting on eroded surface of Crawton basalt at Crawton. The photograph 
shows finer conglomerate filling cracks in the lava. 
Fig. 5. “Sandstone veins ” in basalt on shore near Whistleberry, Kinneff. 
Puate II. 
Geological Map of South-Eastern Kincardineshire, [Geological lines on area north of the Highland 
Boundary fault are taken from maps of H.M. Geological Survey. | 
Prave III. 
Horizontal sections along lines A, B, C, and D of Plate II. 
x. Dalradian schists, Cr.B. Crawton basalt. 
a, Upper Cambrian. _ 0.Ac!. Hypersthene andesite and basalt. 
b. Downtonian. g.-F. Quartz porphyry. 
Lr, Basement breceia of Downtonian. t.D, Teschenite. 
Di. Dictyocaris horizon of Downtonian. M. Quartz dolerite. 
c!, Lower Old Red Sandstone. F, Fault. 
c°, Upper Old Red Sandstone. H.F, Highland fault. 
_V. Volcanic conglomerate and tuffs. T. Vhrust plane. 
Re, Dacite. u. Uneonformity. 
h.Ac', Hornblende and augite Anied 
