San Gabriel Mountains

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The San Gabriel mountain range is a region in Southern California that forms the northern boundary of the Los Angeles basin and provides a number of canyoneering opportunities to the many residents of Los Angeles and surrounding areas. More information

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  The San Gabriel mountain range is a region in Southern California that forms the northern boundary of the Los Angeles basin and provides a number of canyoneering opportunities to the many residents of Los Angeles and surrounding areas.

Character

Most Los Angeles canyons are predominantly granite. The rock can be sharp and crumbly at times, but is often more solid at waterfall pour-overs. Canyons walls can be steep, but are rarely sheer. Most canyons have many trees that may be used as anchors. Many canyons have some water, but few if any present true class C challenges during most of the year.

Closure

Parts of the Angeles National Forest in the San Gabriel Mountains remain closed following the 2009 Station Fire.

External links

• Wikipedia
• Chris Brennen's Adventures in the San Gabriels
• Alpine Training Services' Canyon Beta
• Jason Willis' uCanyon
• Eispiraten forum

Credits

San Gabriel Mountains

Information provided by automated processes. Authors are listed in chronological order.

In all habitats live animals and plants that deserve respect, please minimize impact on the environment and observe the local ethics. Canyoneering, Canyoning, Caving and other activities described in this site are inherently dangerous. Reliance on the information contained on this site is solely at your own risk. There is no warranty as to accuracy, timeliness or completeness of the information provided on this site. The site administrators and all the contributing authors expressly disclaim any and all liability for any loss or injury caused, in whole or in part, by its actions, omissions, or negligence in procuring, compiling or providing information through this site, including without limitation, liability with respect to any use of the information contained herein. If you notice any omission or mistakes, please contribute your knowledge (more information).