Why the Colorado Plateau’s Red Rock Layers Reveal a Long Story of Changing Landscapes
Explore how ancient environments, tectonic uplift and erosion shaped the Colorado Plateau's red rock landscapes.
Explore how ancient environments, tectonic uplift and erosion shaped the Colorado Plateau's red rock landscapes.
How to Read a Landscape on a Geology Field Trip: Six Observations That Matter — An accessible, evidence-led geology feature for readers interested in Earth science and geological history.
The dramatic rock towers of Arizona's Chiricahua region are associated with thick deposits of volcanic ash that cooled and welded together. Later weatherin
The Capitan Reef of West Texas and New Mexico is a major Permian carbonate system preserved around the margins of an ancient basin. Its rocks record a mari
Salt flats develop where water collects in a closed basin and evaporates, leaving dissolved minerals behind. Death Valley's playa surfaces preserve a chang
White Sands in New Mexico is known for its bright dune field, which is unusual because the dunes are made largely of gypsum rather than the quartz sand com
Petrified wood forms when buried plant material is gradually mineralised, preserving aspects of the original wood structure. It is a fossil record of ancie
The Basin and Range Province is recognised by alternating mountain ranges and broad valleys. Much of this pattern developed as the crust stretched and brok
The Rio Grande Rift is an extensive zone where the continental crust of the southwestern United States has been stretched. Its basins, fault scarps and vol
An unconformity is a surface that represents a gap in the geological record. It can form when deposition stops, older rocks are eroded, or both processes o