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Stream Bank Stabilization with Vegetated Gabions

机译:带植被的石笼网的河岸稳定

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摘要

The Merrimack River flows for 115 miles from its source at the confluence of the Pemmigewasset and Winnipesauke Rivers, through central New Hampshire and eastern Massachusetts and into the Atlantic at Newburyport. The Merrimack has a watershed of over 5,000 square miles. Twelve thousand years ago, the nomadic Paleo Indians fished the Merrimack, as it flowed through what is now Manchester, New Hampshire. Around 6,000 years later, the nomadic tribes began settling. These early natives used crude nets across the river to trap the fish. Later, permanent weirs of brush and branches, and eventually stone weirs, trapped the fish and made catching them easier.
机译:梅里马克河在Pemmigewasset河和Winnipesauke河汇合处从源头流过115英里,穿过新罕布什尔州中部和马萨诸塞州东部,并在Newburyport进入大西洋。 Merrimack有一个超过5,000平方英里的分水岭。一万二千年前,游牧的古印第安人在梅里马克(Merrimack)流经新罕布什尔州曼彻斯特的那一天钓鱼。大约6000年后,游牧部落开始定居。这些早期的当地人使用粗网穿过河来捕捞鱼。后来,永久的灌木丛和树枝堰,最终是石堰,将鱼困住,使捕捞变得更加容易。

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