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DTSTAMP:20260518T091620
DTSTART;TZID=America/Detroit:20260626T090000
DTEND;TZID=America/Detroit:20260626T170000
SUMMARY:Exhibition:Resistance is Fertile: Celebrating 30 Years of Cultivating Change
DESCRIPTION:Resistance Is Fertile honors the founding moment of the Institute for Research on Women & Gender\, while speaking to the present. The institute was established because faculty members believed that research on women\, gender\, and sexuality required an institutional commitment to thrive. That belief was itself a form of resistance—to disciplinary silos\, to marginalization\, to the idea that such scholarship was peripheral.\n\nThis theme reminds us that resistance is not merely reactive\; it is constructive. When rooted in collaboration and sustained through infrastructure\, it produces knowledge that reshapes disciplines\, institutions\, and public life.\n\nThis exhibit celebrates 30 years of IRWG—its history\, its programs\, and the people whose vision and labor built it into what it is today. Through archival materials\, milestones\, and stories\, we trace the evolution of an institute that has continually expanded the boundaries of research in women\, gender\, and sexuality.\n\nThis exhibit centers growth\, collaboration\, and intellectual creativity—honoring the sustained efforts\, bold ideas\, and collective care that have shaped IRWG’s legacy and continue to guide its future.\n\nHosted and sponsored by the Institute for Research on Women and Gender and the Department of Women’s and Gender Studies\, U-M. \n\nLocated on the first floor of Lane Hall (204 S. State Street)\, the Exhibit Space is free and open to the public\, M-F\, 9am-4pm.
UID:148280-21903729@events.umich.edu
URL:https://events.umich.edu/event/148280
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:Gender Based Violence,gender,Activism,women's studies,Women's And Gender Studies,Women History,women
LOCATION:Lane Hall
CONTACT:
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BEGIN:VEVENT
DTSTAMP:20260508T155502
DTSTART;TZID=America/Detroit:20260626T090000
DTEND;TZID=America/Detroit:20260626T200000
SUMMARY:Exhibition:The People’s Bicentennial
DESCRIPTION:This selection of original artifacts documents the work of the Peoples Bicentennial Commission (PBC)\, which challenged the official\, corporate-sponsored commemoration of the 1976 bicentennial. This year we celebrate the 250th anniversary of the signing of the Declaration of Independence.\n\nItems on display are from the Joseph A. Labadie Collection\, which documents social protest movements and radical history.\n\nHOURS\nSunday 2-8pm\nMonday-Thursday 9am-8pm\nFriday 9am-4pm\nSaturday 11am-5pm
UID:147925-21902460@events.umich.edu
URL:https://events.umich.edu/event/147925
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:History,Library,Free
LOCATION:Hatcher Graduate Library - Hatcher Gallery Exhibit Room (1st floor)
CONTACT:
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BEGIN:VEVENT
DTSTAMP:20260604T121400
DTSTART;TZID=America/Detroit:20260626T100000
DTEND;TZID=America/Detroit:20260626T110000
SUMMARY:Workshop / Seminar:10 Week Accessibility Challenge
DESCRIPTION:Join the 10-Week Accessibility Challenge to learn more about accessibility basics\, best practices\, and U-M resources and tools available to help you with this work. This training program is open to all U-M staff\, faculty\, and students - no prior accessibility experience or knowledge is required. These live sessions dive deeper into the Challenge content and give participants a chance to get live support and ask questions with our digital accessibility staff. If you have any questions or concerns\, please reach out to accessibility-challenge@umich.edu.\n\nThe 10-Week Accessibility Challenge sessions take place on Fridays at 10:00 - 11:00am\, June 5 - August 7\, 2026. Due to the July 3 holiday\, the Challenge will be moved to July 2.
UID:148367-21904015@events.umich.edu
URL:https://events.umich.edu/event/148367
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:Workshop,Virtual,Inclusion,Disability,Digital Accessibility,Accessibility
LOCATION:Off Campus Location
CONTACT:
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BEGIN:VEVENT
DTSTAMP:20260527T121530
DTSTART;TZID=America/Detroit:20260626T100000
DTEND;TZID=America/Detroit:20260626T120000
SUMMARY:Class / Instruction:Faculty Master Class: Amir Eldan\, cello
DESCRIPTION:Center Stage Strings (CSS) – one of SMTD’s MPulse performing arts summer programs for youth – welcomes the public to attend as SMTD Professor Amir Eldan presents a master class on cello.\n\nCSS develops the talents of serious young classical music students in the areas of solo and chamber music performance.\n\nFACULTY BIO\n\nhttps://smtd.umich.edu/profiles/amir-eldan/
UID:148177-21903191@events.umich.edu
URL:https://events.umich.edu/event/148177
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:Talk,Faculty,Free,Music,North Campus,Workshop
LOCATION:Earl V. Moore Building - Britton Recital Hall
CONTACT:
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BEGIN:VEVENT
DTSTAMP:20260618T141338
DTSTART;TZID=America/Detroit:20260626T110000
DTEND;TZID=America/Detroit:20260626T120000
SUMMARY:Lecture / Discussion:Bryanne Gordon Dissertation Defense
DESCRIPTION:Click here to join via zoom: https://umich.zoom.us/j/97057153103 (password is rhyolite)\n\nHigh-SiO2 (>75 wt%) rhyolites are the most differentiated silicate magmas on Earth and are relatively scarce in the volcanic rock record\, especially at subduction zones. This scarcity may be due to their narrow (<50°C) liquidus-solidus interval\, which promotes extensive crystallization over small drops in temperature\, preventing eruption. However\, high-SiO2 rhyolites do erupt\, sometimes in supervolcano quantities (≤1000 km 3 )\, in regions of continental extension (e.g.\, Yellowstone\, WY and Long Valley\, CA). Therefore\, understanding the magmatic architecture (i.e.\, temperature/pressure prior to eruption) and/or processes that enable successful eruption of high-SiO2 rhyolite are critical to investigate.\n\nOne of the greatest challenges in studying high-SiO2 rhyolites is the paucity of mineral- melt thermometers\, barometers and hygrometers that can be accurately applied to them. This leads to conflicting results when thermometers and hygrometers calibrated on different magma compositions are applied to high-SiO2 rhyolites. Also\, it is often not possible to use one of the only reliable thermometers\, which is based on the equilibrium between two Fe-Ti oxides\, because of post-eruptive alteration. In Chapter 2\, a new biotite-melt thermometer is presented. New biotite-melt equilibrium experiments were conducted on high-SiO2 rhyolite between 675-800 °C and P H2O = 225-125 MPa. These experimental data were combined with biotite analyses in natural high-SiO2 rhyolites\, for which high-quality Fe-Ti two-oxide temperatures are available (660-800 °C)\, to calibrate the new thermometer. It was successfully deployed on four Jurassic high-SiO2 rhyolite dikes\, which contained pristine biotite\, demonstrating its utility on samples for which Fe-Ti two-oxide thermometry is not possible.\n\nIn Chapter 3\, the biotite-melt and Fe-Ti two-oxide thermometers were applied to a suite of high-SiO2 rhyolite domes and flows (from Glass Mountain\, CA)\, which preceded a climactic\, supervolcano eruption. A puzzling feature of these rhyolites is their highly variable phenocryst abundances (<1 to 20%)\, despite little change in their major-element compositions. One sample grew ~8% phenocrysts at a remarkably low temperature (660 ± 10 °C)\, which is below the water-saturated solidus at upper crustal conditions (≤300 MPa). Three hypotheses were tested to explain the variable phenocryst abundances: (1) they reflect equilibrium temperature\, pressure\, and melt H2O contents during crystal growth in magmatic reservoir(s)\, (2) the H2O-saturated granitic solidus is lower than previously documented\, or (3) rapid phenocryst growth\, following a kinetic delay to nucleation\, occurred during magma ascent. Based on new experiments\nconducted in this chapter\, along with documented phenocryst compositions and textures\, it shown that phenocrysts in the Glass Mountain high-SiO2 rhyolites grew during dike transport to the surface and not in a magma chamber.\n\nIn Chapter 4\, U-Pb zircon crystallization ages (162-169 Ma) were obtained on a high-SiO2 rhyolite dike swarm in the Sierra Nevada\, CA\, which dates an episode of extension within the long-lived Mesozoic arc. These results are unexpected for two reasons: (1) this age range overlaps a magmatic flare-up Sierra Nevada arc (145-175 Ma)\, and (2) they differ from\npreviously published K-Ar ages for these dikes (168-209 Ma)\, which overlaps a lull in Sierran arc magmatism. However\, the zircon ages for the dike swarm directly overlap the age (160-170 Ma) of the Coast Range Ophiolites\, which formed in the forearc region due to trench-parallel spreading. This may have induced shearing and extension in the main Sierran arc.
UID:149048-21905355@events.umich.edu
URL:https://events.umich.edu/event/149048
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:Dissertation,Earth And Environmental Sciences
LOCATION:1100 North University Building - 2540
CONTACT:
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