Mr. William Holwell, the nephew, was of course a Fellow of Exeter College. He travelled through France and Italy about the year 1780, where he began forming a collection of pictures, bequeathed on his decease to the National Gallery. He is said to have taken Orders with some reluctance, for the purpose of accepting this valuable living. But the most important event in this gentleman’s life was his marrying Charlotte, daughter and heiress of James Carr, Earl of Erroll. He in consequence assumed the name of Carr. He died in the year 1830, having survived his wife nearly twenty years, who has a monument to her memory in Menheniot church. In the valuation of Pope Nicholas, the name of this parish is written Manyhinyhet, or Saihinet, proofs of the small reliance that can be placed on mere phonic etymologies. Cartuther, noticed by Mr. Hals, became the property and the residence of the Morsheads, but having been sold, with all the other possessions of that family, it was purchased by Mr. Kekewich. Mr. Lysons gives a detail of other manors and bartons of little interest. This parish has the reputation of being the most fertile of corn, especially of wheat, in the whole county. The aspect of the church town gives a strong impression of monastic remains, but there is not any tradition on record of a religious establishment in the place. Menheniot measures 6047 statute acres. Annual value of the Real Property, as £. _s._ _d._ returned to Parliament in 1815 10599 0 0 Poor Rate in 1831 1422 11 0 Population, { in 1801, | in 1811, | in 1821, | in 1831, { 918 | 1024 | 1170 | 1253 giving an increase of 36½ per cent. in thirty years. GEOLOGY, BY DOCTOR BOASE. The southern part of this parish is bounded by the hill of Clicker Tor, which is entirely composed of a dark compact serpentine, abounding in steatite, asbestos, tremolite, and other magnesian minerals. The occurrence of this large mass of serpentine, amidst an extensive tract of rocks belonging to the calcareous series, imparts no little geological interest to this parish, which deserves therefore to be more minutely examined; for the cursory observations hitherto published have not satisfactorily developed the connection of this serpentine with the adjoining rocks. In crossing the parish from north to south, the rocks are first seen to consist of compact felspar and hornblend, resembling those at Rosecradock in St. Clear; next they become more schistose, and the hornblend forms only the colouring material, as it does on the north of Leskeard town; at Pengover the hornblend again abounds, and is intermixed with calcareous spar, as in the vicinity of St. Ives. Approaching the church of Menheniot, the rocks again put on the appearance of a true hornblend schist, and this is succeeded by the serpentine of Clicker Tor. THE EDITOR.