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Welcome to the Snake River Boating Guide

This is a free project from boaters for boaters. Everybody can contribute and add her/his information and experiences to the Snake River Boating Guide to make boating on the Snake easier, safer and even more fun.

The guide can be searched (1) by map, (2) by a list of all marinas, parks, landings, anchorages, locks and dams, or (3) by searching the entire page content. Detailed maps allow to georeference points of interest and to check out the surrounding areas. Sections of NOAA charts help to orient the boater.

As you can see this site is still under construction but we will work on new features and we'll add more info and point of interests asap after they have been submitted.

 

We hope you have fun with the free Snake River Boating Guide,

Christian and friends

 

 
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You want to get your dogs out of the water when they are done with swimming? Cap'n Crash shows how! Works for small and large puppies ;-)  

 
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Please help to improve the free Snake River Boating Guide. If we all contribute this guide will help to make boating on the Snake safer and more fun.

If you had a great time on the Snake, discovered some neat spots for boating or fishing and want to share please submit it here.

Also if you encountered a dangerous spot (shoal, sandbar, obstructions etc.) please let your fellow boaters know and report it here.

 

 
Snake River History PDF Print E-mail
Written by Christian   
Wednesday, 02 December 2009 17:55

The Snake River is a major river in the greater Pacific Northwest in the United States. It is the largest and longest tributary of the Columbia River, which is the largest North American river that empties into the Pacific Ocean. Rising in western Wyoming, the river flows westwards through the Snake River Plain, and turns north to empty into the Columbia at the Tri-Cities area of the state of Washington, draining 108,000 square miles (280,000 km2) in parts of six U.S. states. The river is 1,040 miles (1,670 km) long, and its average flow is 56,900 cubic feet per second (1,610 m3/s).

 

Steep mountains, low hills, deep canyons and predominantly, the flat alluvium of the Snake River Plain characterize the geologically diverse and active watershed of the Snake River. The plain originates from a large volcanic hotspot below the North American Plate, which now lies underneath Yellowstone National Park, the headwaters of the Snake River.

 

Gigantic flooding episodes that occurred during the previous Ice Age, involving glacially formed lakes spilling into the middle and lower Snake River, carved out Hells Canyon, the Palouse Hills, and many other topographical features along the middle and lower Snake. Two of these catastrophic flooding events affected the river. Pluvial Lake Bonneville spilled catastrophically into the Snake River Plain about 14,500 years ago. The Missoula Floods also played a role in the shaping of the lower Snake's watershed, although its effects were more pronounced along the Columbia River. As far back as 11,000 years, tribes of prehistoric Native Americans lived along the length of the Snake. Salmon from the Pacific Ocean traveled up the Columbia River and into the Snake River, often numbering in the millions. These fish were central to the lives of the people that lived along the Snake below Shoshone Falls.

 

By the time the Lewis and Clark Expedition crested the Continental Divide and sighted the valley of the Snake's major tributary, the Salmon River, the Nez Perce and Shoshone were the most powerful tribes along the Snake River. At this time, contact with Europeans introduced horses to Snake River Plain tribes, reshaping their lifestyles for the next few hundred years before American settlement of the area. Later American explorers and British fur trappers from the Hudson's Bay Company further changed and utilized the resources of the Snake River basin. At one point, a hand sign made by the Shoshone Indians representing fish was misinterpreted to represent a snake, giving the Snake River its name.

 

Source: Wikipedia

 

Last Updated on Wednesday, 17 February 2010 23:10
 

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