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See also: term loosely used by geologists when speaking generally of any stratum or deposit which contains bones of whatever kind
.
It is also applied to those brecciated and stalagmitic deposits on the floor of caves, which frequently contain osseous remains
.
In a more restricted sense it is used to connote certain thin layers of bony fragments, which occur upon well-defined See also: geological horizons
.
One of the best-known of these is the See also: Ludlow See also: Bone See also: Bed, which is found at the See also: base of the Downton See also: Sandstone in the Upper Ludlow series
.
At Ludlow itself, two such beds are actually known, separated by about 14 ft. of strata
.
Although quite thin, the Ludlow Bone Bed can be followed from that See also: town into See also: Gloucestershire for a distance of 45 M
.
It is almost made up of fragments of spines, teeth and scales of ganoid See also: fish
.
Another well-known bed, formerly known as the " See also: Bristol " or " See also: Lias " Bone Bed, exists in the See also: form of several thin layers of micaceous sandstone, with the remains of fish and saurians, which occur in the Rhaetic Black Paper Shales that lie above the See also: Keuper marls in the See also: south-west of See also: England
.
It is noteworthy that a similar bone bed has been traced on the same geological See also: horizon in See also: Brunswick, See also: Hanover and See also: Franconia
.
A bone bed has also been observed at the base of the Carboniferous See also: limestone series in certain parts of the south-west of England
.
BONE-LACE, a kind of lace made upon a cushion from See also: linen thread; the See also: pattern is marked out with pins, round which are See also: twisted the different threads, each wound on its own bobbin
.
The lace was so called from the fact that bobbins were formerly made of bone
.
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