Dr. Latisha Brengman
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Granular iron formation thin section image
Carbonate crystals in granular iron formation
Warped, zoned carbonate crystal
Distribution of the element silicon in iron formation sample
Underground physics lab
Underground physics lab
Taconite mine
Mine microbes
Underground physics lab
Entrance to Soundan Underground Mine
Desert sunset
North shore volcanics ~1.1 Ga
Gunflint trail stromatolites
@NORDSIMS
LT and the 1280
Geologists geologizing
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Latisha Ashley Brengman
ph. (218) 726-7586
e. lbrengma@d.umn.edu

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Department of Earth and Environmental Sciences
1114 Kirby Drive, 221 Heller Hall
Duluth, MN 55812

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The University of Minnesota Duluth’s Land Acknowledgment: "We collectively acknowledge that the University of Minnesota Duluth is located on the traditional, ancestral, and contemporary lands of Indigenous people. The University resides on land that was cared for and called home by the Ojibwe people, before them the Dakota and Northern Cheyenne people, and other Native peoples from time immemorial. Ceded by the Ojibwe in an 1854 treaty, this land holds great historical, spiritual, and personal significance for its original stewards, the Native nations and peoples of this region. We recognize and continually support and advocate for the sovereignty of the Native nations in this territory and beyond. By offering this land acknowledgment, we affirm tribal sovereignty and will work to hold the University of Minnesota Duluth accountable to American Indian peoples and nations." Learn more here: https://www.d.umn.edu/about-umd/campus-history/land

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Diana Sahy@DianaSahy·
22 Sep

Seafloor sediments (quartz, micas, etc.) cemented by ~5,000 year old methane-derived aragonite needles, from ~300 metres below sea level off the coast of Norway. U-Th dating by @isotopesUK, photo by @BgsSem. Field of view ~200 x 100 μm.

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