Crews begin underwater search of Henrys Fork near St. Anthony for missing BYU-I student
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EastIdahoNews.com file photo June 2020
ST. ANTHONY – Search and rescue crews are preparing for an underwater dive as day four of the search for a missing Brigham Young University-Idaho student resumes along the Henrys Fork of the Snake River in St. Anthony.
Matthew Rios, 22, of Peru got caught in the current and floated downstream after jumping off the Fun Farm Bridge with two of his friends Thursday afternoon. Rios’ friends made it safely to shore. A third friend was also there who did not get in the water, according to a mom who declined to give her name.
Authorities release name of BYU-I student missing in Henrys Fork
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Fun Farm Bridge at 699 North 2650 East in St. Anthony. | Courtesy Freearenas.com
ST. ANTHONY – We now know the name of the Brigham Young University-Idaho student who jumped off a bridge into the Henrys Fork of the Snake River Thursday afternoon.
Fremont County Sheriff Len Humphries tells EastIdahoNews.com 22-year-old Matthew Rios from Peru and two of his friends were swimming and jumped off the Fun Farm Bridge at 699 North 2650 East in St. Anthony around 3:30 p.m.
Rios’ friends made it safely to shore, but he got caught in the current and floated downstream. Authorities continue to search for him Saturday.
Authorities searching for BYU-I student who is presumed drowned in the Henrys Fork
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Fun Farm Bridge at 699 North 2650 East in St. Anthony. | Courtesy Freearenas.com
ST. ANTHONY – A search is underway for a missing Brigham Young University-Idaho student who jumped off a bridge in St. Anthony Thursday afternoon and is presumed to have drowned.
Fremont County Sheriff Len Humphries tells EastIdahoNews.com that a male student and two of his friends jumped off the Fun Farm Bridge at 699 North 2650 East while swimming in the Henrys Fork of the Snake River. It happened around 3:30 p.m.
Two of the friends swam back to shore, while the other got caught in the current and floated downstream.
reconstructed from sub-ice shelf and offshore sediments
J.A. Smith; C.-D. Hillenbrand; C. Subt; B.E. Rosenheim; T. Frederichs .
Abstract:
Because ice shelves respond to climatic forcing over a range of time
scales, from years to millennia, an understanding of their long-term
history is critically needed for predicting their future evolution. We
present the first detailed reconstruction of the Larsen C Ice Shelf (LCIS),
eastern Antarctic Peninsula (AP), based on data from sediment cores
recovered from below and in front of the ice shelf. Sedimentologic and
chronologic information reveals that the grounding line (GL) of an expanded
AP ice sheet had started its retreat from the midshelf prior to 17.7 ± 0.53