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Secretary of Agriculture report on watersheds

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Item’s are ‘child’ level descriptions to ‘parent’ objects, (e.g. one page of a whole book).

  • 26 APPALACHIAN AND WHITE MOUNTAIN WATERSHEDS. north to Mount Webster on the south, and includes the following peaks: Madison, the three Adamses, Jefferson, Clay, Washington, Monroe, Franklin, Pleasant Dome, Clinton, and Webster. This stretch of country is about 15 miles long by 5 miles in breadth and contains about 50,000 acres. This range is the source of five rivers, by which it is drained—the Saco, the Ammonoosuc, and Israel, tributaries of the Connecticut, and the Moose and Peabody, tributaries of the Androscoggin. The underlying rock is. granitic gneiss. By disintegration and mixture with organic matter it forms a loamy sand. The depth of the soil varies with the elevation, aspect, and gradient. In the valleys and on the lower slopes the soil is generally deep, with little outcropping rock. With ascent in altitude and increase in gradient the depth increases, till on the steep upper slopes there are only immense masses of bare outcropping rock and scattered bowlders. Next to the Presidential Range, the Carter-Moriah Range is of the most importance. It runs parallel to the Presidential Range and is separated from it by the Glen Ellis and Peabody rivers. The highest peak is Carter Dome, with an elevation of 4,860 feet, and there are eight peaks in all, with elevations of over 4,000 feet. The general character of the soil and underlying rock is the same as on the Presidential Range. The range is about 20 miles long and from 2 to 7 miles wide. It is entirely surrounded by the five rivers by which it is drained—the Peabody and Glen Ellis rivers on the west, the Wild and the east branch of the Saco on the east and south, and the Androscoggin on the north. The Peabody and Wild rivers flow northeast into the Androscoggin, and the Glen Ellis flows into the Saco. The northern part of the White Mountain region, in Coos County, N. H., is flatter than the White Mountains proper, and contains many lakes and low mountains with wide rolling valleys between. The Connecticut Lakes, the headwaters of the Connecticut River, lie in the northern part of this region. These lakes are small. The protection of the watershed around them is therefore of greater importance than if they were large and formed a greater storage area for water. The area in Maine includes 700,000 acres in Oxford and Franklin counties. This entire region is very rough and rugged, containing no regular ranges of mountains, but being broken up into a great number of irregular peaks and ridges. The five Rangeley' lakes, the headwaters of the Androscoggin River, lie in the southern part of this region. North of these lakes, in the Magalloway, Cufsuftic, and Ken- nebago watersheds, the country is extremely rough, including a great number of tall mountain peaks, extending up to the Boundary Mountains between the United States and Canada. The extreme eastern portion of this area lies in the Dead River watershed, the extreme headwaters of a tributary of the Kennebec River. The land in this watershed is flatter than to the west and contains many small lakes, ponds, and bogs. For this reason the protection of the watersheds is not of so great importance as in the more mountainous country to the west, and the main watershed of the Kennebec River has not, therefore, been included in the proposed boundary lines.
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Object’s are ‘parent’ level descriptions to ‘children’ items, (e.g. a book with pages).