GSA today : a publication of the Geological Society of America
The evolution of creationismJohn Perry's neglected critique of Kelvin's age for the Earth: A missed opportunity in geodynamicsZealandia: Earth’s Hidden ContinentCelestial driver of Phanerozoic climate?Impacts, mega-tsunami, and other extraordinary claimsUnderstanding the Great Ordovician Biodiversification Event (GOBE): Influences of paleogeography, paleoclimate, or paleoecologySubduction of the Chile Ridge: Upper mantle structure and flowCanada's craton: A bottoms-up viewEvidence for life in a martian meteorite?Gaia and the colonization of Mars.Reply: The extinction of the dinosaurs in North AmericaWHEN THE CONTINENTS CREPT AWAYAre we now living in the AnthropoceneCO2 as a primary driver of Phanerozoic climateLand transformation by humans: A reviewThe Extinction of the Dinosaurs in North AmericaThe subduction factory: How it operates in the evolving EarthThe significance of sheeted dike complexes in ophiolitesThe 1906 earthquake and a century of progress in understanding earthquakes and their hazardsAre plutons assembled over millions of years by amalgamation from small magma chambers?Is agriculture eroding civilization's foundation?Rock Stars Thomas Chrowder Chamberlin (1843–1928)Enigmatic boulder trains, supraglacial rock avalanches, and the origin of “Darwin's boulders,” Tierra del FuegoPersistent Holocene Outflow from the Black Sea to the Eastern Mediterranean Contradicts Noah's Flood HypothesisNew evidence for abrupt climate change in the Cretaceous and Paleogene: An Ocean Drilling Program expedition to Shatsky Rise, northwest PacificStromatolites and MISS—Differences between relativesTurbulent lifestyle: Microbial mats on Earth's sandy beaches—Today and 3 billion years agoSpeciation collapse and invasive species dynamics during the Late Devonian “Mass Extinction”A human-induced hothouse climate?Future volcanism at Yellowstone caldera: Insights from geochemistry of young volcanic units and monitoring of volcanic unrestThe Rheic Ocean: Origin, Evolution, and SignificanceTropical shoreline ice in the late Cambrian: Implications for Earth's climate between the Cambrian Explosion and the Great Ordovician Biodiversification EventThe heavy metal contamination of Lake Junín National Reserve, Peru: An unintended consequence of the juxtaposition of hydroelectricity and miningImpact of erosion, sedimentation, and structural heritage on the structure and kinematics of orogenic wedges: Analog models and case studiesIs the Anthropocene an issue of stratigraphy or pop culture?: COMMENTMoving lithospheric modeling forward: Attributes of a community computer codeA bird’s-eye view of geology: The use of micro drones/UAVs in geologic fieldwork and educationPenrose Conference Scheduled: Low δ18O rhyolites and crustal melting: Growth and redistribution of the continental crustA Scientific Sabbatical on Capitol HillFeedbacks between Science and Policy: Do they exist?
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GSA today : a publication of the Geological Society of America
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GSA Today
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA Today
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA Today
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GSA Today
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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GSA today : a publication of the Geological Society of America
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1991-01-01T00:00:00Z