Issues
Articles
Polymorphic transformations of titanium oxides contribute to economic uranium mineralization in sandstone
Disconformity-controlled hydrothermal dolomitization and cementation during basin evolution: Upper Triassic carbonates, UAE
Ice? Salt? Pressure? Sediment deformation structures as evidence of late-stage shallow groundwater in Gale crater, Mars
Exceptional preservation of a marine tapeworm tentacle in Cretaceous amber
Okanogan lobe tunnel channels and subglacial floods into Moses Coulee, Channeled Scabland, northwestern United States
Rehydrated glass embayments record the cooling of a Yellowstone ignimbrite
Landscapes on the edge: River intermittency in a warming world
Evidence for ca. 1 Ga hypervelocity impact event found in northwest Greenland
Bedrock rivers are steep but not narrow: Hydrological and lithological controls on river geometry across the USA
Subsidence-induced early doming at a large ignimbrite caldera
Bank strength variability and its impact on the system-scale morphodynamics of the upper Amazon River in Brazil
Oligocene melting of subducted mélange and its mantle dynamics in northeast Asia
A little mica goes a long way: Impact of phyllosilicates on quartz deformation fabrics in naturally deformed rocks
Alkenone-derived estimates of Cretaceous pCO2
Scoria cone erosional degradation by incision: Different behaviors in three volcanic fields reflect environmental conditions
Bacterial magnetofossil evidence for enhanced Pacific Ocean respired carbon storage during buildup of Antarctic glaciation
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Cover Image
Cover Image
COVER: Margin of the Greenland Ice Sheet in the exposed foreland in Inglefield Land, northwestern Greenland. Multiple detrital impact melt rocks were retrieved at this and other locations along the ice wall or within glaciofluvial channels, all recently emerged from under the ice. All but one of the radiometrically dated samples record a Late Paleocene impact event attributed to the proximal 31-km-wide Hiawatha Impact Structure; however, a single pebble-sized sample contains evidence of a second, ancient hypervelocity impact event that occurred in the Paleoproterozoic, around one billion years ago. (Coordinates: 78.58920, –66.81570, looking north.) See “Evidence for ca. 1 Ga hypervelocity impact event found in northwest Greenland,” by William Hyde et al., p. 517–521..
Photo by Pierre Beck
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