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THE winter of 1786-87 set in very early. At Warren, in Maine, on the fourteenth of November the St. George's river was frozen so hard and thick that the ice bore horses and sleighs as far down as Watson's Point, and on the following day to the mouth of the stream. It did not break up until the latter part of the following March. The sloop Warren, lying at the wharf in Thomaston and loading with a cargo for the West Indies, was frozen in and compelled to remain there all through the winter. By the twentieth of November, the harbor of Salem, Mass., was frozen over as far out as Naugus Head; and the Connecticut river was congealed so quickly that, at Middletown in that state, within twenty-four hours after boats passed over it the ice had become strong enough to bear heavy weights and people were driving on it with their horses and sleighs. Frozen into the river were between thirty and forty vessels that had been prepared for their voyages, the masters expecting to sail before the river was closed by ice. The month of December was unusually severe, and snow storms came frequently and terrifically, great quantities of snow covering the earth to a depth that impeded travel in all portions of the country. The remainder of the winter was also severe, and in the vicinity of Rockland, Me., snow remained on the ground as late as April 10, so deep and hard-crusted that teams passed over the fences in every direction without obstruction.

CoCoRaHS is an acronym for the Community Collaborative Rain, Hail and Snow Network. CoCoRaHS is a unique, non-profit, community-based network of volunteers of all ages and backgrounds working together to measure and map precipitation (rain, hail and Snow). By using low-cost measurement tools, stressing training and education, and utilizing an interactive Web-site, our aim is to provide the highest quality data for natural resource, education and research applications.

A COLD northeast storm of wind, rain and snow raged along the coast of New England during the latter part of March, 1830, producing a great tide, which in some parts exceeded the highest tide remembered there. The storm began on the morning of Friday, the twenty- sixth, and continued till one o'clock in the afternoon, the tide being at its height at noon of that day.