The geology of New HampshireA report comprising the results of explorations ordered by the legislature . ain in the east part ofMoultonborough, thence through the east part of Tuftonborough to apoint one half mile south of Upper Beech pond, around which it passes,running north-east to a point about one mile east of Water Village. The place where this water-shed line approaches nearest to Lake Win-nipiseogee is west of Upper Beech pond, one of its bays being here threemiles distant. The farthest point that is drained into Winnipiseogee isthat last named, being on the north side of Batson pond,

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The geology of New HampshireA report comprising the results of explorations ordered by the legislature . ain in the east part ofMoultonborough, thence through the east part of Tuftonborough to apoint one half mile south of Upper Beech pond, around which it passes,running north-east to a point about one mile east of Water Village. The place where this water-shed line approaches nearest to Lake Win-nipiseogee is west of Upper Beech pond, one of its bays being here threemiles distant. The farthest point that is drained into Winnipiseogee isthat last named, being on the north side of Batson pond, seven milesfrom the lake. Thence it follows nearly the north-east and south-east boundaries ofWolfeborough to Mt. Delight, passing within one mile of Smiths it extends south through the west part of Brookfield, over Crop-pie Crown mountain, thence south-west through New Durham, nearlyto Downings mills, passing one mile south-east from Merry-meeting the course again turns south to the west corner of Farmington,then south-east three miles to the Blue Hills range, which it follows. 7 x^}i^^^0^-^WA !^< rrtlead M»9 Jni^r Ip8- f 5l-^;l?r sale- .?<aC?<**?-i^ySfi;3jS^ ^\^^ 1;

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