The relics collected here are:--Flint objects in considerable abundance, among which were two saws, a lance-head, and a beautiful knife-flake (=Fig. 50=, No. 1), now in the Museum at Varese; fragments of coarsely-made dishes without handles or ornamentation. Three canoes, roughly made and similar to those from Mercurago, were found at a depth of 8 feet. One of the canoes, 7 feet long, was presented to the Museum at Varese. Along with these objects were bones of the stag, goat, and roe. (B. 171.) TORBIERA DI VALCUVIA. In 1870 Professor Leopoldi Maggi described the remains of a palafitte found in "un bacino torboso" between Santa Maria di Cuveglio and Cavona. (B. 187.) This basin lies among glacial _débris_, and was formerly a small lake, but in modern times it became entirely filled up with peat. On the surface there was a layer of vegetable soil 10 inches thick, then spongy peat to the depth of 3 feet, and then a layer of more solid peat about 1 foot 8 inches thick. Underneath these layers was a blackish muddy deposit, extending to an unknown depth, into which the piles were inserted. These piles were from 5 to 10 feet long, and 8 to 10 inches in diameter. They were closely set, and along with them were several beams lying horizontally. The relics consisted of pottery, knives of bronze and iron, charcoal, etc., all of which were dispersed. TORBIERA DI BRENNO. Another locality that has yielded interesting remains, of "stazioni palustri," is the "torbiera di Brenno-Useria," situated along the road from Varese to Porto Ceresio, on Lake Lugano. Here, some years ago, a canoe was dug out by the peat-cutters, and associated with it were a large number of weapons of bronze and iron, bracelets, fibulæ (=Fig. 51=, No. 14), bones of domestic animals and of man, but no objects of flint. (B. 327, p. 92.) LAKE OF LECCO. As early as 1860 Desor thought he had discovered indications of a palafitte in Lake Maggiore,[39] but this was subsequently disproved, and up to the present time no remains of these ancient dwellings have been found in this lake. The explanation of their absence in the larger lakes of Italy is to be found in the physical conditions of these glacial and rock-cut basins, which, owing to the depth of water and their rapidly-shelving shores, afford no holding for piles.