Thin Remains (2022)
The “walls” featured here are the remains of a hardened magma-filled fracture called a dike. This dike formed underground when minette magma rose through cracks associated with the Shiprock volcanic system about 30 million years ago. Later, erosion stripped away the softer surrounding sedimentary rocks, leaving the dike standing as a narrow wall and the main volcanic conduit standing as Tsé Bitʼaʼí (Shiprock Pinnacle).
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