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Mill Brook (Swift River tributary) facts for kids

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Mill Brook
Mill Brook (Swift River tributary) is located in New Hampshire
Mill Brook (Swift River tributary)
Mill Brook (Swift River tributary) is located in the United States
Mill Brook (Swift River tributary)
Country United States
State New Hampshire
County Carroll
Towns Sandwich, Tamworth
Physical characteristics
Main source White Mountain National Forest
1,560 ft (480 m)
43°54′15″N 71°23′28″W / 43.90417°N 71.39111°W / 43.90417; -71.39111
River mouth Swift River
Tamworth
438 ft (134 m)
43°50′4″N 71°14′53″W / 43.83444°N 71.24806°W / 43.83444; -71.24806
Length 10.7 mi (17.2 km)
Basin features
Tributaries
  • Right:
    Hoag Brook

Mill Brook is a cool stream, or small river, in the beautiful White Mountains of New Hampshire, United States. It flows for about 10.7 miles (17.2 kilometers). This stream is like a smaller helper river, called a tributary, that flows into the Swift River.

Mill Brook is part of a bigger system of waterways. This system includes the Bearcamp River, Ossipee Lake, and the Saco River. All these waters eventually flow into the Atlantic Ocean.

Where Does Mill Brook Start?

Mill Brook begins high up on the southern side of a mountain called Mount Whiteface. This mountain is located in a town named Sandwich. The water starts flowing from an elevation of about 1,560 feet (475 meters) above sea level.

From its start, the brook flows mostly towards the southeast. It travels through the town of Sandwich.

Mill Brook's Journey

As Mill Brook flows, it makes its way into another town called Tamworth. The brook continues its journey through the pretty landscapes of New Hampshire.

Along its path, Mill Brook collects water from smaller streams. One of these smaller streams that joins Mill Brook is called Hoag Brook.

Where Does Mill Brook End?

Mill Brook's journey ends when it reaches the Swift River. This meeting point is in Tamworth, just east of a small village called Whittier.

When Mill Brook joins the Swift River, it is at a lower elevation of about 438 feet (133 meters) above sea level. This means the water has flowed downhill quite a bit from its source.

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