• Rainbow over Half Dome

    Yosemite

    National Park California

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  • Road Closures Due to El Portal Fire

    The Big Oak Flat Road between Crane Flat and the El Portal Road is temporarily closed. There is no access to Yosemite Valley via the Big Oak Flat Road or Highway 120. Tioga Road is open and accessible via Big Oak Flat and Tioga Pass Entrances. More »

  • Campground Closures Due to Fire

    Crane Flat, Bridalveil Creek, and Yosemite Creek Campgrounds are temporarily closed. More »

  • Yosemite National Park is Open

    Yosemite Valley, Glacier Point, and Wawona/Mariposa Grove areas are open and accessible via Highways 140 and 41. Tioga Road is not accessible via Highways 140 and 41 due to a fire.

Tenaya Lake Area Plan

Tenaya Home

Timeline

Information

Comment




The Finding of No Significant Impact was released in May 2011
Visit the PEPC webpage to review the document.


 
Image of Tenaya lake and surrounding granite cliffs and domes.

               

                   

Tenaya Lake is a magnificent High Sierra lake surrounded by granite domes, lodgepole forests, and Yosemite’s vast wilderness. It is the largest lake in Yosemite’s front-country. Because of its remarkable scenic qualities, its inviting blue water, and its proximity to Tioga Road, Tenaya Lake is one of the most popular destinations for summer visitors in Yosemite.

Problems associated with visitor use, visitor safety, and resource impacts have been occurring for decades. Thanks to a grant from The Yosemite Fund, a comprehensive analysis of, and solution to these issues is underway.

The environmental assessment was available for review and comment, beginning October 12, 2010 and ending November 17, 2010. The document is still available on the Planning, Environment, and Public Comment (PEPC) webpage for review.

Did You Know?

View of Yosemite Valley from the Wawona Tunnel Vista.

Rockfall events have helped shape many of the outstanding features along Yosemite Valley's walls, including Royal Arches, North Dome, and Half Dome. Giant talus slopes that slant away from the Valley walls accumulate debris with each rockfall event.