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Connecticut River Oxbow in Northampton Earthcache EarthCache

This cache has been archived.

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Difficulty:
1.5 out of 5
Terrain:
3 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

I am in the process of getting one of Massachusett's first Earthcaches resurrected. More to follow. Please bear with me while I iron out the details. Thanks! ~WMC

Coordinates will take you to the Summit House in J.A. Skinner State Park. Entrance to Park is off Mountain Road off route 47. Upper half of road is uphill and twisty with a hairpin turn. You can park at e


One of the best areas to view the oxbow is from the Summit House porch, southwest corner. This is part of the Mt. Holyoke Range / Joseph Allen Skinner State Parks. The present Summit House is built on the site of the first summit house in North America. There are many trails in the area including the M and M trail, and caches. The park is open from 10 to 6. On weekends and holidays there is a $2,00 fee to drive to the top and park. You can walk, bike and ride horseback the trails at any time. The road past the Halfway house, where you can park and take the Halfway House trail to the top, is uphill and winding with hairpin turns. The park entrance, a infomation kiosk and parkng is on Mountain Road off of Route 47.

20,000 years ago the last glacier, which covered this area under a mile of ice, formed a dam near Rocky Hill, CT. This dam created what is called Lake Hitchcock. This lake covered most of the Connecticut River Valley under 200 feet of water and extended 150 miles north into Vermont. About 10,000 years ago the dam broke. Since then the CT river has been meandering over the old lake bed. All rivers flow in a sinuous pattern, depending on many factors: the climate. the shape of the channel,the erodibilty of the surrending landscape,the amount of warer, and its velocity. If the riverbank is made of erodible material, the force of the water tends to cut it away. On the opposite side of the river, the current is slower and sediments settle out and build up. Over time the curves grow larger and develop into enormus loops. Eventually the land between the loops erode away and the river loop is cutoff and an oxbow lake is formed. In 1840 this happened in Northampton and shortened the river's length by 3.5 miles. To claim credit you must submit, along with your log, a picture of you, a team member or your gps, with the oxbow in the background like my picture. If you can't submit a picture, at the park entrance there is a information kiosk with a bird on it, email me what the bird is.

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