SEC. 10.] NORTH-WESTERN KTJTCH. &33 



Near the base of the hill on its south-eastern side, some bright 

 Ashy beds in the up- S^^^^ ^^^^ looking beds with red bands mottled 

 per Jurassic group. ^^^^^ ^^^^ greatly the appearance, but perhaps 



not quite the thickness, of the steeply dipping faulted beds of the 

 section above given, p. 230. They are here nearly horizontal with a 

 low inclination to the south-west, and, as in the other locality, contain 

 scattered grains of quartz. They rest upon a very soft coarse greenish 

 sandstone. 



Above these unusual beds is a compact speckled slightly calcareous 

 _g , ., . buff grit, over which a gray compact calcareous 



Jurassic beds. ^^^^ about a foot thick, occurring at the north- 



ern foot of Uttra hill, contains a layer or two crowded with broken 

 shell fragments and small fragmentary Beletnnites. The beds here dip 

 to the south at about 5°, and are almost immediately overlaid by the 

 lowest portion of the Liekka and Uttra traps, consisting of sandy looking 

 concretionary ash, with low unsteady dips to the south and south by 

 west. 



The unconformity of these traps upon the Jurassic beds is not appre- 

 ciable on the spot, but seen from the small trap hill to the north-west 

 becomes very apparent. 



Just at the village of Goonaree and near it, strong light-coloured 

 Fault bringing in the sandstones variegated with red, ferruginous bands 

 nummuUtic beds. ^^^ grayish flaggy shales form a small anticlinal 



to the westward, and are contorted along the fault which brings into 

 junction with them the vertical white and yellowish marly nummulitic 

 beds, showing as a narrow band along the margin of the Runn. 



A mass of basaltic trap occurs in this fault about a mile from 

 Goonaree to the east-south-east. 



( 233 ) 



