A paleocontinent or palaeocontinent is a distinct area of continental crust that existed as a major landmass in the geological past. Sandstone. Most sandstone is composed of quartz or feldspar because these are the most common minerals in the Earth's crust.
Sandstone is part of the History of Earth.
Determine if the claim is supported, refuted, or if there is not enough information based on the evidence.

Claim: A paleocontinent or palaeocontinent is a distinct area of continental crust that existed as a major landmass in the geological past. Sandstone. Most sandstone is composed of quartz or feldspar because these are the most common minerals in the Earth's crust.

Evidence: Sandstone is part of the History of Earth.

Options: 

 - supported

 - refuted

 - not enough information
not enough information
Determine if the claim is supported, refuted, or if there is not enough information based on the evidence.

Claim: A paleocontinent or palaeocontinent is a distinct area of continental crust that existed as a major landmass in the geological past. Sandstone. Most sandstone is composed of quartz or feldspar because these are the most common minerals in the Earth's crust.

Evidence: Sandstone is part of the History of Earth.

Options: 

 - supported

 - refuted

 - not enough information
user
not enough information
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