plains deformation belt
Quick Summary
Plains deformation belts are geological features found on Venus, primarily in low-lying areas like Lavinia Planitia and Atalanta Planitia. These belts are characterized by less pronounced relief compared to mountain belts and show evidence of parallel folding and faulting, suggesting they form through compression, deformation, and uplift of the planet's lithosphere. They often appear as parallel bands spaced hundreds of kilometers apart within a given lowland region. These features are a result of tectonic activity, which deforms the planet's crust.1
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