FOSSIL SHELLS FREESTONE. 7 
Cornua ammonis are very common about tliis village. As we 
were cutting an inclining path up the Hanger, the labourers found 
them frequently on that steep, just under the soil, in the chalk, 
and of a considerable size. In the lane above Well-head, ui the 
way to Emshot, they abound in the bank, in a darkish sort of 
marl, and are usually very small and soft : but in Clay's Pond, a 
little further on, at the end of the pit, where the soil is dug out 
for manure, I have occasionally observed them of large dunen- 
sions, perhaps fourteen or sixteen inches in diameter. But as 
these did not consist of firm stone, but were formed of a kind of 
terra lapidosa, or hardened clay, as soon as they were exposed to 
the rains and frost they mouldered away. These seemed as if 
they were a very recent production. In the chalk-pit, at the north- 
west end of the Hanger, large nautili are sometimes observed. 
In the very thickest strata of our freestone, and at consider-, 
able depths, weU-diggers often find large scallops or pectines, 
having both shells deeply striated, and ridged and furrowed alter- 
nately. They are highly mipregnated with, if not wholly com- 
posed of, the stone of the quarry 
LETTER IV To T. PENNANT, Esa. 
As in a former letter the freestone of this place has been only 
mentioned incidentally, I shall here become more particular. 
This stone is in great request for dearth-stones, and the beds 
of ovens : and in lining of lime-kilns it turns to good account ; 
for the workmen use sandy loam instead of mortar ; the sand of 
which fluxes,* and runs by the intense heat, and so cases over 
the whole face of the kiln with a strong vitrified coat like glass, 
that it is well preserved from injuries of weather, and endures 
thirty or forty years. When chiseled smooth, it makes elegant 
fronts for houses, equal in colour and grain to the Bath stone ; 
and superior in one respect, that, when seasoned, it does not 
scale. Decent cliimney-pieces are worked from it of much closer 
and finer grain than Portland ; and rooms are floored with it, but 
it proves rather too soft for this purpose. It is a freestone, 
cutting in all directions, yet has something of a grain parallel 
Ro that it can hardly be expected that an}- sort of ammal, tl)e exuviae of which occur in the 
(secondary) chalk, can he still founJ in existence at the prpsent time. — En. 
• There may probably be also in the chalk itself thv<t is burnt for lime a proportion of snn*!, 
tor few chalks are so pure as to have none. 
