Color: Fossil
Hill Chert ranges in color from off white to bluish white. Hues
include red, pink, yellow and green. Speckled with oxides and
quartz.
Texture: Medium to very fine grain
Luster: Waxy to vitreous
Silica Fabrics / Fossils: Macro fossils
include brachiopods, bryozoans, colonial corals echinoderms, and
stromatoporoids. Micro fossils include navifusa and
polyedryxium are present
Patina: When weathered it becomes white and
may have staining of shades of yellow or red.
Heat Treatment:
Knapping:
Notes: Fossil Hill Chert can be distinguished
from Onondaga Chert by the presences of Hapsidopalla in Onondaga Chert.
It is similar in characteristics to Bois Blanc Formation Chert, however,
Fossil Hill Chert has Navifusa and Polyedryxium which is absent in Bois
Blanc Formation Chert.
Distribution:
Distribution Comments:
Fossil Hill Chert is associated with the Fossil Hill Formation Limestone
with primary sources being located in Redwing Ontario. Primary
outcroppings are found in Bruce and Grey counties, Ontario. Found into
New York.
Projectile point made from this material:
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