Glacial Pass Concretions
AKA: Glacier Pass Siliceous Mudstone











Natural Form:



Description of Physical Characteristics:

Color:  Glacial Pass Concretions has a dark gray cortex with a dark gray outer layer and a light brown chalky center.  Artifacts tend to utilize the outer layer with colors ranging from dark gray or brown brown to beige, and greyish brown with some purplish brown.  Silica veins may be present.

Texture:
Medium to fine grain

Luster: Waxy

Translucency: Opaque

Silica Fabrics / Fossils: Present

Patina: Milky grayish brown

Heat Treatment:  Heat treatment does not change the flaking quality, but increases the luster from waxy to vitreous and produced reddish or purple hues.

Knapping: 
 

 

 

 

 

 

 

 

 

 

 

  

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Distribution:
Glacial Pass Concretions is thought to be associated with the Fernie Formation of Alberta.  It occurs in nodule eroded from the shale in the eastern edge of the Rocky Mountains in Alberta. 
Projectile point made from this material:



Heat treated


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References: (See Reference Page, Entry Number):

Similar Material:
Commonly made projectile point from this material:

Archaeological Context: