68 MISCELLANEOUS NOTES. 
NOTE—LEPIDOPTERA. 
xodia palustrana part Halifax: a Species New to Yorkshire.— 
On val Ist last, I took a Tortrix on eign Neagnn: which was quite new to 
me, and on the 8th, aa a diligent arse got four more. One of them I ba 
to Capitals Thompson, of Lon o kin ndly secéruined the name for me as 
ixodia palustrana Zell., and informed Pa that “oye pga had been considered 
almost yee a Scotch in S quite the Scotts of York. 
PAR ROBIN eee Street, “Bridge ‘End. Restiick. 't eb. 6th, 18 
ixoadta pal trana is a very good eo al 7 the ‘List of Yorkshire 
pr eroe a? but besides in Scotland, we belie ax been reported from 
one or two localities in the north of England. ae r. 
NV — OLLUSCA. 
Limnza glutinosa in Lincolnshire.—Of this — -snail I f , 
last month, eg Salecty All “Saints, in the lar, arge ‘drain’ or hee ay by the 
side of the road between Saltf tby Station and th . It is an addition to 
Mr. Roe nek’s List d Freshw; ollusca of Lincolnshire, 
published in ‘ The ‘ogaeroagid in 1887, but it was referred to by the author, 1 
his prefatory remarks, as a species which might q wey possibly be found in the 
sg go I ap ave submited the sell for 8 gga gir Eg to Mr. Taylor, 
e this record uniform in va Roebuck’s list as 
per goecific racteriatiatin. pas WALLIS kw. umtaay sth, 1 1894 
NOTE—MAMMALIA. 
elanic Specimen of - Long-eared Bat.—I have — se. ig? 
to record the occurrence of an interesting and, I believe, not a ety 0) of 
us), W 
i ize. 
above was dark silvery grey, with a fulvous ines ; ve: pale mouse grey } 
wings, face, and ears eg sepia brown, almost The extent of the wings 
was nine inches.—WM. EaGLe CLARKE, Eanes "February 1 1893. 
ee or OLOGY. 
cee not met with any pee description of the 
bib oton granite of Foxdale, in Oe I ie - Man, and it may, therefore, be 
worth wi o draw attention to the very cl sablane of t this rock to the 
Leinster granites, an exhaustive study of whieh was given by Prof. Sollas a few 
ears 
In han wi -specimens it is seen = be a etapa so po grey muscovite- 
granite. The brown mica is rdinate in quantity to the white, occurs 
chiefly as little patches ecietoned in the latter. Quartz i D abidsdant, and its grains 
r i par. 
€ peculiarities are explained by a thin section of the rock examined 
e bro ica is i 
a a “pa ag grains of isotope garnet, and indeed an occasional little crystal . 
ed in some hand-specimens.—ALFRED HARKER 
St Ten’ s College, Canieline February 15th, 1894. no 
Naturalist, 
i 
