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Issues
Channel-levee evolution in combined contour current-turbidity current flows from flume tank experiments: REPLY
Elda Miramontes; Joris T. Eggenhuisen; Ricardo Silva Jacinto; Giovanni Poneti; Florian Pohl; Alexandre Normandeau; D. Calvin Campbell; F. Javier Hernández-Molina
Geology August 01, 2020, Vol.48, e508. doi:https://doi.org/10.1130/G47885Y.1
Why do large, deep rivers have low-angle dune beds?: REPLY
Geology August 01, 2020, Vol.48, e506. doi:https://doi.org/10.1130/G47882Y.1
Why do large, deep rivers have low-angle dune beds?: COMMENT
Jim Best; Julia Cisneros; Renato Paes de Almeida; Cristiano Galeazzi; Marco Ianniruberto; Hongbo Ma; Christopher Unsworth; Thaiënne van Dijk
Geology August 01, 2020, Vol.48, e505. doi:https://doi.org/10.1130/G47578C.1
Channel-levee evolution in combined contour current–turbidity current flows from flume-tank experiments: COMMENT
Geology August 01, 2020, Vol.48, e507. doi:https://doi.org/10.1130/G47508C.1
Articles
Using speleothems to constrain late Cenozoic uplift rates in karst terranes
Geology April 29, 2020, Vol.48, 755-760. doi:https://doi.org/10.1130/G47466.1
Late Miocene sediment delivery from the axial drainage system of the East Carpathian foreland basin to the Black Sea
Geology May 12, 2020, Vol.48, 761-765. doi:https://doi.org/10.1130/G47318.1
Halogens in hydrothermal sphalerite record origin of ore-forming fluids
Max Frenzel; Nigel J. Cook; Cristiana L. Ciobanu; Ashley D. Slattery; Benjamin P. Wade; Sarah Gilbert; Kathy Ehrig; Mathias Burisch; Max R. Verdugo-Ihl; Panagiotis Voudouris
Geology May 12, 2020, Vol.48, 766-770. doi:https://doi.org/10.1130/G47087.1
Evidence for glacial geological controls on the hydrology of Maine (USA) peatlands
Geology May 12, 2020, Vol.48, 771-776. doi:https://doi.org/10.1130/G46844.1
Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation
Geology May 18, 2020, Vol.48, 777-781. doi:https://doi.org/10.1130/G47377.1
Onset of permanent Taklimakan Desert linked to the mid-Pleistocene transition
Geology May 12, 2020, Vol.48, 782-786. doi:https://doi.org/10.1130/G47406.1
The genesis of a giant mud canopy by catastrophic failure of a thick evaporite sealing layer
Geology May 12, 2020, Vol.48, 787-791. doi:https://doi.org/10.1130/G47430.1
Modulation of zircon solubility by crystal–melt dynamics
Geology May 12, 2020, Vol.48, 798-802. doi:https://doi.org/10.1130/G47405.1
Overpressure release: Fluid inclusion evidence for a new mechanism for the formation of heavy oil
Geology May 18, 2020, Vol.48, 803-807. doi:https://doi.org/10.1130/G47227.1
A 1000-yr-old tsunami in the Indian Ocean points to greater risk for East Africa
Vittorio Maselli; Davide Oppo; Andrew L. Moore; Aditya Riadi Gusman; Cassy Mtelela; David Iacopini; Marco Taviani; Elinaza Mjema; Ernest Mulaya; Melody Che; Ai Lena Tomioka; Elisante Mshiu; Joseph D. Ortiz
Geology May 12, 2020, Vol.48, 808-813. doi:https://doi.org/10.1130/G47257.1
Tracing shock-wave propagation in the Chicxulub crater: Implications for the formation of peak rings
Geology May 18, 2020, Vol.48, 814-818. doi:https://doi.org/10.1130/G47129.1
A sub-centennial-scale optically stimulated luminescence chronostratigraphy and late Holocene flood history from a temperate river confluence
Geology May 18, 2020, Vol.48, 819-825. doi:https://doi.org/10.1130/G47079.1
Northern-sourced water dominated the Atlantic Ocean during the Last Glacial Maximum
Geology May 19, 2020, Vol.48, 826-829. doi:https://doi.org/10.1130/G47628.1
Toxic mercury pulses into late Permian terrestrial and marine environments
Geology May 19, 2020, Vol.48, 830-833. doi:https://doi.org/10.1130/G47295.1
Rapid cooling of the Rustenburg Layered Suite of the Bushveld Complex (South Africa): Insights from biotite 40Ar/39Ar geochronology
Geology May 10, 2020, Vol.48, 834-838. doi:https://doi.org/10.1130/G46865.1
Experimental evidence for crustal control over seismic fault segmentation
Geology May 18, 2020, Vol.48, 844-848. doi:https://doi.org/10.1130/G47115.1
Forum
Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation: COMMENT
Geology June 11, 2020, Vol.48, e509. doi:https://doi.org/10.1130/G47946C.1
Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation: REPLY
Geology June 11, 2020, Vol.48, e510. doi:https://doi.org/10.1130/G47984Y.1
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Cover Image
Cover Image
![issue cover]()
COVER: A tsunami hit the coastline of Tanzania 1000 yr ago, destroying an ancient Swahili fishing village whose ruins were found close to the modern town of Pangani. The human skull in the image, one of many remains found at the site, testifies to the unexpected destruction that occurred during the tsunami. These remains represent the oldest tsunami victims thus far found in East Africa. See “A 1000-yr-old tsunami in the Indian Ocean points to greater risk for East Africa” by Maselli et al., p. 808–812.
Photo by: Vittorio Maselli
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