The Birch Mountains kimberlite field is a kimberlite field in Northern Alberta, Canada. It is a product of kimberlite volcanism during the Cretaceous period which was the most prolific period for worldwide kimberlite volcanism. The field is part of the Northern Alberta kimberlite province and consists of 8 diatremes and is younger than the nearby Buffalo Head Hills kimberlite field, dating approximately 75 million years.[1]
The diatremes within the field include: