The Ross orogeny was a mountain building event in Antarctica in the early Paleozoic.
The ancestral (also termed proto-) Trans-Antarctic Mountains were uplifted earlier by the Beardmore orogeny but had eroded as a broad epicratonic sea flooded much of Antarctica in the Cambrian.
Shallow water sedimentary rocks, platform carbonates and deepwater turbidites from this period are found in the mountain range.
The Ross orogeny was one of the most extensive orogenic events in Antarctica, causing widespread plutonism and metamorphism.
Bimodal magmatism and extension mark the beginnings of the orogeny, while during the later phase sedimentary rocks at the continental margin were deformed, metamorphosed and intruded with granite batholiths.