This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
Out of stock
This fossilized charcoal is a rare witness to the precise moment of the cataclysm that marked the beginning of the extinction of the dinosaurs.
This fossilized material comes from forest residues, rich in iridium, charred following a giant meteorite impact in the Yucatan Peninsula ~65 million years ago.
Outcrops of the K-T (Cretaceous-Tertiary) boundary rich in this lignite have appeared in different regions of Mexico in the Sierra Madre Oriental.
This lignite is currently protected and therefore rare to find on the market.
Out of stock
This fossilized charcoal is a rare witness to the precise moment of the cataclysm that marked the beginning of the extinction of the dinosaurs.
This fossilized material comes from forest residues, rich in iridium, charred following a giant meteorite impact in the Yucatan Peninsula ~65 million years ago.
Outcrops of the K-T (Cretaceous-Tertiary) boundary rich in this lignite have appeared in different regions of Mexico in the Sierra Madre Oriental.
This lignite is currently protected and therefore rare to find on the market.
Out of stock
This fossilized charcoal is a rare witness to the precise moment of the cataclysm that marked the beginning of the extinction of the dinosaurs.
This fossilized material comes from forest residues, rich in iridium, charred following a giant meteorite impact in the Yucatan Peninsula ~65 million years ago.
Outcrops of the K-T (Cretaceous-Tertiary) boundary rich in this lignite have appeared in different regions of Mexico in the Sierra Madre Oriental.
This lignite is currently protected and therefore rare to find on the market.
Out of stock
This fossilized charcoal is a rare witness to the precise moment of the cataclysm that marked the beginning of the extinction of the dinosaurs.
This fossilized material comes from forest residues, rich in iridium, charred following a giant meteorite impact in the Yucatan Peninsula ~65 million years ago.
Outcrops of the K-T (Cretaceous-Tertiary) boundary rich in this lignite have appeared in different regions of Mexico in the Sierra Madre Oriental.
This lignite is currently protected and therefore rare to find on the market.
This fossilized charcoal is a rare witness to the precise moment of the cataclysm that marked the beginning of the extinction of the dinosaurs.
This fossilized material comes from forest residues, rich in iridium, charred following a giant meteorite impact in the Yucatan Peninsula ~65 million years ago.
Outcrops of the K-T (Cretaceous-Tertiary) boundary rich in this lignite have appeared in different regions of Mexico in the Sierra Madre Oriental.
This lignite is currently protected and therefore rare to find on the market.
Out of stock
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
Out of stock
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
Out of stock
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
Out of stock
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
Out of stock
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
Out of stock
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
This clay is the witness of the impact of the meteorite that contributed to the extinction phenomena of the dinosaurs.
It is located between the Cretaceous and the Tertiary (Bidart marl and Danian limestone).
Out of stock
This fossilized charcoal is a rare witness to the precise moment of the cataclysm that marked the beginning of the extinction of the dinosaurs.
This fossilized material comes from forest residues, rich in iridium, charred following a giant meteorite impact in the Yucatan Peninsula ~65 million years ago.
Outcrops of the K-T (Cretaceous-Tertiary) boundary rich in this lignite have appeared in different regions of Mexico in the Sierra Madre Oriental.
This lignite is currently protected and therefore rare to find on the market.