San Francisco Peak Obsidian
(Fremont Peak - Agassiz Saddle)












Natural Form:



Description of Physical Characteristics:

Color:  San Francisco Peak Obsidian is grayish black and extremely vitrophyric with abundant feldspar phenocrysts and inter-banded with ash.  The cortex ranges from a ashy rhyolite to weathered black.

Texture:


Luster:

Translucency

Silica Fabrics / Fossils: 

Patina:

Heat Treatment: 

Knapping:  Poor quality knapping material not allowing for controlled fractures.  More vitreous material may have a slightly improved knapping quality.

 

 

 

 

 

 

 

 

 

 

  

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Distribution:
Distribution Comments:
San Francisco Peaks Obsidian is associated with the San Francisco Volcanics and occurs as abundant nodules above 3,300m in elevation on the northwest slope of Fremont Peak near Agassiz Saddle in the Coconino National Forest, Coconino County, Arizona.
Projectile point made from this material:



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References: (See Reference Page, Entry Number):

Similar Material:
Commonly made projectile point from this material:

Archaeological Context:
Not known in archaeological contexts.
.