r > a «d the 



e. Al 



on* 







rare 



8 of 



' &e pel,. 



sl H and, 

 distinctly 



clear and 

 at varioti 



nains, age 



sharpness, 



-11 general 



by a thin 



nanner ii 





he clay in 

 much 0: 



cias occur 

 •ocks ; and 

 d bouWec 



f this kind 



j ordinaij 



1 belie* 



long c* 

 nagniW* 

 1C rock I 



ide ' a Ji 



>r fart 



1 



nes 



an 



i 



e, 







rH 



PERMIAN BRECCIAS. 



25 



//« 



101. — From Howler's Heath, south end of the Malvern upper 

 Ills. These show, on a small scale, the general nature of Ga ^ k _ ut « 



the brecciated conglomerate, viz., the angularity of the • T « ble ; cas f 1 



* 111 xVCCOSS 3il-« 



stones, and the red marly paste in which they are embedded. 



102. — Berrow Hill, near Hartley, Abberley Hills. 



103. — Abberley Hills, behind Hundred House. 



104. — Clenty north of Bromsgrovc. 



105. — Wars Hill, near Bewdley. 



106. — Romsley, near the Day House, Bromsgrove, Lickey, 

 These specimens were dug from the quarries and loosened 

 to show the angularity of the smaller fragments. 



107 — Part of a grooved small boulder (of altered Cam- 

 brian grit) dug out of a quarry, Berrow Hill, near Martley, 



\, and the Wo 



The rubbing and grinding of the stone 



goes 



partly round the edge marked 



X ; in this respect 

 resembling the side of the stone marked X, from the glacial 



-almost Ik drift, No. 93. 



108. — SUBANGULAR PURPLE FINE CAMBRIAN GRIT Scratch- 



ed 071 all sides ; Six Ashes, 



Enville 



The scratches run chiefly with the length of the stone, 

 but many of them cross each other in all directions. Com- 

 pare with No. 35, from the glacier of the Grindelwalcl; 

 52, from the Vosges ; 67, 76, from the moraines of Caer- 

 narvonshire ; 83, 86, and 87, from the moraine drift ; and 



90 and 91, from the ordinary marine glacial drift of An- 

 glesea. 



109. — Subangular stone (Cambrian grit), scratched, 

 the scratches covered with a thin ferruginous coating ; from 

 the outlier of Church Hill, Bay ton. This small outlier is 

 entirely surrounded by Coal-measures, which lie on the Old 

 red sandstone. The nearest spot where grit like this stone 

 occurs in place is the Longmynd. The scratches at X show 

 a tendency to pass round the curved edge as in 93 and 107. 



110.— Part of a subangular stone (Cambrian grit?), 



Hi 



111. 



(Cambrian grit),/ 



atcd ; Bromsley, near Day House, Bromsgrove Lickey. 



