368 REPORT—1896. 
Striated Surfaces. 
On roadside 4 mile from Raby towards Willaston— 
Planed surface of sandstones striated from N. 40° W. (true). Two other patches 
near with the same direction of striation. 
Well Lane, Rock Ferry— 
On roadside, planed surface covered with boulder-clay, striated from N. 25° W. 
LANCASHIRE. 
Reported by Mr. J. Lomas, A.2.C.S., per Glacialists’ Association. 
Liverpool, the Dingle Shore— 
1 granite, from Goat Fell, Arran. 
Reported by Mr. W. Parker, per Glacialists’ Association. 
Facit near Rochdale. Out of sewer-excavation opposite Co-operative 
Stores— 
*] Eskdale granite. 
Near Long Acres Farm— 
*] quartz syenite ; *2 Buttermere granophyre. 
1 local sandstone ; 1 sandstone ; *1 andesite ; 1 rhyolite. 
* All these are stated to have lain with their long axes N.W.-S.E. 
Robin Hood Clough— 
1 rhyolite. 
Whitworth. In sewer-cutting, near Whitworth Manufacturing Company’s 
Mills— 
1 Carboniferous Limestone with coral (? Syringopora). 
LINCOLNSHIRE. ! 
Communicated by the Lincolnshire Boulder Committee. 
Reported by the Rev. W. Tuckwett, JA. 
Waltham— 
1 basalt (Whin Sill) ; 1 basalt. 
Louth— 
The ‘Blue Stone’ basalt; 1 basalt; 1 light red granite. 
Louth, chalkpit north of chwrch—Large heap of boulders, averaging 
9 inches diameter, included the following varieties :— 
Rhomb-porphyry ; augite-syenite; lamprophyre; diorite; gneiss; pink 
granite ; white granite; quartz-porphyry, Carboniferous Limestone, and 
Lias. 
Louth, brickyard on Road to Elkington—Boulders and pebbles in 
heaps include the following :— 
Rhomb-porphyry ; augite-syenite ; porphyrite (? Fredericsvaarn); halleflinta; 
mica schist; schist; black flint; green-coated flint; porphyrite; fine- 
grained white granite; quartz-porphyry ; diorite; basalt ; vesicular lava ; 
conglomerate (with pebbles of quartz-porphyry); Millstone Grit; Car- 
boniferous Limestone ; Carboniferous sandstone (gannister) ; ironstone 
(2? Liassic) ; Septarian nodule (? Kimeridge clay). 
1 This report will be published in extenso in the Vaturalist. 
