See also:physical geography, a
See also:ridge or bunched
See also:mound of
See also:gravel or sand, " tumultuously stratified," occurring in connexion with glacial deposits, having been formed at the mouths of tunnels under the ice . When the ice-
See also:sheet melts, these features, formerly concealed by the glacier, are revealed . They are
See also:common in the glaciated portions of the
See also:lower Scottish valleys . By some authorities the
See also:term " kame," or specifically "
See also:serpentine kame," is taken as synonymous with "
See also:esker," which however is preferably to be applied to the long mound deposited within the ice-tunnel, not to the bunched mound at its mouth .
KAMENETS PODOLSKIY, or PODOLIAN KAMENETS (Polish Ka...
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