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Issues

ISSN 0091-7613
EISSN 1943-2682
In this Issue

Articles

Geology April 13, 2020, Vol.48, 643-648. doi:https://doi.org/10.1130/G47126.1
Geology April 13, 2020, Vol.48, 649-653. doi:https://doi.org/10.1130/G47202.1
Geology April 13, 2020, Vol.48, 654-657. doi:https://doi.org/10.1130/G47238.1
Geology April 17, 2020, Vol.48, 658-662. doi:https://doi.org/10.1130/G47301.1
Geology April 17, 2020, Vol.48, 663-667. doi:https://doi.org/10.1130/G47451.1
Geology April 17, 2020, Vol.48, 668-672. doi:https://doi.org/10.1130/G47235.1
Geology April 27, 2020, Vol.48, 673-677. doi:https://doi.org/10.1130/G47201.1
Geology April 27, 2020, Vol.48, 678-682. doi:https://doi.org/10.1130/G47096.1
Geology April 29, 2020, Vol.48, 683-687. doi:https://doi.org/10.1130/G46733.1
Geology April 17, 2020, Vol.48, 688-692. doi:https://doi.org/10.1130/G47410.1
Geology April 27, 2020, Vol.48, 693-697. doi:https://doi.org/10.1130/G47223.1
Geology April 27, 2020, Vol.48, 698-702. doi:https://doi.org/10.1130/G47054.1
Geology April 27, 2020, Vol.48, 703-707. doi:https://doi.org/10.1130/G47211.1
Geology April 27, 2020, Vol.48, 708-712. doi:https://doi.org/10.1130/G47467.1
Geology April 29, 2020, Vol.48, 713-717. doi:https://doi.org/10.1130/G47171.1
Geology April 29, 2020, Vol.48, 718-722. doi:https://doi.org/10.1130/G47521.1
Geology April 29, 2020, Vol.48, 723-727. doi:https://doi.org/10.1130/G47280.1
Geology April 29, 2020, Vol.48, 728-732. doi:https://doi.org/10.1130/G47400.1
Geology April 29, 2020, Vol.48, 733-736. doi:https://doi.org/10.1130/G47411.1
Geology April 29, 2020, Vol.48, 737-741. doi:https://doi.org/10.1130/G47253.1
Geology April 29, 2020, Vol.48, 742-747. doi:https://doi.org/10.1130/G47172.1
Geology May 18, 2020, Vol.48, 748-752. doi:https://doi.org/10.1130/G47346.1

Forum

Geology July 01, 2020, Vol.48, e503. doi:https://doi.org/10.1130/G47627C.1
Geology July 01, 2020, Vol.48, e504. doi:https://doi.org/10.1130/G47858Y.1
  • Cover Image

    Cover Image

    issue cover

    COVER: Broken blocks of glacier ice that were heavily rounded in the process of glacier detachment (pencil in image is ~15 cm long). Together with rock clasts, they are firmly embedded in a matrix of muddy ice that was pulverized during the detachment and then reconsolidated upon deposition. See Jacquemart et al., “What drives large-scale glacier detachments? Insights from Flat Creek glacier, St. Elias Mountains, Alaska” p. 703–707.

    Photo by: Mylène Jacquemart

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