(3.) We find that the second form of the Cornish name, namely, _cara clowse in cowze_, may either be a merely metamorphic corruption of _cara cowz in clowze_, readily suggested and supported by the new meaning which it yielded of “gray rock in the wood;” or, even if we accept it as an original name, that it would be no more than a name framed by the Cornish-speaking monks of the Mount, in order to embody the same spurious tradition which had given rise to the name of “Hore rock in the wodd.” I need hardly add that in thus arguing against Mr. Pengelly’s conclusions, I do not venture to touch his geological arguments. St. Michael’s Mount may have been united with the mainland; it may, for all we know, have been surrounded by a dense forest; and it may be perfectly possible geologically to fix the date when that forest was destroyed, and the Mount severed, so far as it is severed, from the Cornish coast. All I protest against is that any one of these facts could be proved, or even supported, by the Cornish name of the Mount, whether _cara cowz in clowze_, or _cara clowse in cowze_, or by the English name, communicated by William of Worcester, “the Hore rock in the wodd,” or finally by the legend which gave rise to these names, and which, as can be proved by irrefragable evidence, was transplanted by mistake from the Norman to the Cornish coast. The only question which, in conclusion, I should like to address to geologists, is this: As geologists are obliged to leave it doubtful whether the insulation of St. Michael’s Mount was due to the washing of the sea-shore, or to a general subsidence of the country, may it not have been due to neither of these causes, and may not the Mount have always been that kind of half-island which it certainly was two thousand years ago? 1867. XVI. BUNSEN.(97)