Final answer:
The fossil tracks of a Permian cow-size lizard can be found in the Kaibab Limestone, which is a geological formation deposited during the Permian period. These tracks provide important information about the ancient reptile's behavior and environment.
Step-by-step explanation:
The fossil tracks of a Permian cow-size lizard can be found in the b. Kaibab Limestone. The Kaibab Limestone is a geological formation that was deposited during the Permian period, which occurred between 299 and 252 million years ago. This formation contains fossils of various organisms, including the tracks of a cow-size lizard. The limestone layers preserve the tracks and provide important clues about the ancient reptile's behavior and environment.