Io YORKSHIRE NATURALISTS IN. MID-RIBBLESDALE. 
Rubus leucostachys. Salix rugosa. 
Rubus lindleianus. Salix ni 
Rubus salteri. Salix phillyreifolia. 
Rubus rosaceus. (Salix laurina 
Rosa subcristata. Potamogeton densus 
Rosa dumetorum. Allium oleraceum 
Myriophyllum spicatum. Scirpus sylvaticus. 
Hippuris vulgaris. Scirpus pauciflorus. 
Sedum villosum. Schcenus nigricans. 
Pimpinella magna. Avena pratensis. 
Sium angustifolium. Equisetum sylvaticum. 
Myrrhis odor. Ophioglossum 
Pulicaria dysenterica Epipactis purpurata. 
Eupatorium cannabinum Lycopus europeu 
eracium m m. Caltha palustris 
Hieracium sylvaticum. Paris quadrifolia. 
Hieracium umbellatum. Primula farinosa. 
Mentha rubra. Pinguicula. 
Mentha sativa. Lysimachia nummularia. 
Symphytum tuberosum. Parnassia palustris. 
Rumex aquaticus. Tris foetidissima 
Salix helix (rubra). 
Mosses. 
Tortula intermedia. Hypnum molluse 
ypnhum rugosum. Hypnum csibki chikdaniies 
The district is described as a promising one for pasture fungi, but it 
was too early in the season. Thirty species were collected, but 
either September or October would be the time for making a 
typical list. 
For the Geological Section, Mr. W. Lower Carter, M.A., F.GS., 
one of the secretaries, writes as follows :— 
The geologists assembled at Chatburn Station, at 11.35, under 
the leadership of Mr. R. H. Tiddeman, M.A., F.G.S., whose work 
on the Ordnance sire) had rendered him aber hecaee with 
the district. The first place visited was the Bold Venture Quarry 
just outside of Chatburn Station, where the chipeiitebs Limestone 
is extensively worked. e s in this quarry are tilted up at 
a high angle, and as the boulder clay, which covers the eastern 
slope of the hill, is removed, the surface of the limestone is shown 
to be smoothed and scored by glacial action, the markings showing 
a movement of the glacier from the north-east. At the other end of 
the quarry a good example of slickenside was seen, due to the 
movement of the beds along a line of fracture. The party then 
walked along the road to Sawley Abbey, but were disappointed in 
not being able to see the upturned limestone strata to be seen in the 
river-bed when the water is low. A slight diversion was made for 
the examination of a limestone quarry on the hillside, which showed 
Naturalist, 
