description of the rocks 
ports Whamside, and Ingleborough, and Penyghent rests , 
and shells, large and small worn 1 f ^ ° ne COntain ’ atnon g corals 
well as through the mas's of 
^4 n ca e „ n e m h „: e j rt; z zzzrzz and c r nly 
reeled Assures, joints, and laminar, of the supporting slaZwTth tl" 
horizontal beds and vertical joints of the limestone entablature! 
meet tZZ “ Z'Z 
the' anldL Td 7„dZ aZZZ“ hZd^Z Ze ~ 
cLaZrof Zrzrt s th°e ne h“°Zs at d ? nite ansks; ^ »- 
ledge of solid geometry suffices to determine ZfoZof “he"'" k "°' V ; 
crystal of slate. — But on entering the next qua r ° S '' PP ° Sed 
observed in the measures, and by prosecuting L iZ TZ" 3410 " ^ 
pass to the other extreme, and believe that all this ? " 6 com nionly 
illusory. Three horizontal floors of fin " a i ed “TaT® U 
in Leek Beck near Kirby Lonsdale in ,f 33 Z ,t Z "T"^ 
on one of these existed four sets of m,- H i ’ , 1 aS found that 
two, the one couple crossin, - at 1 P Z rfge * arran S ed and 
right angles. OneZ TZ s!ts of IZ " 2 “ * he ” U “ at 
it was found to be crossed bv tl 1 ti S " &S considered tlie cleavage, 
115°. On another slab the Z rS " ° f 47 " 90 ” a " d 
90"; in the third they were 54", goZd' iJT** “ a '' 8 ' ,eS ° f 44 ” and 
In the extensive quarries above Imdeton tl,o ,.i OQ 
serve one constant course to the S. E„ dipping slightly' to theTw” 
aoss joints run vertically to the N„ and oblique joints dip N E Th ‘ 
stone is mostly of a fine texture and green colour within ih Z 
often purple on the surfaces; but a hard granular not tl V tl0ugh 
caned -gal, lard, .sometimes intervenes in el^ed 
