The Organic Geochemistry Laboratory at UIC
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    • OGL in the news
  • Photos
    • Paleokarsts and sediment fills
    • Coring Douglas Lake (Michigan)
    • Antarctica 2002: CORING THE LAKES
    • Antarctica 2005: VIDA 1
    • Antarctica 2010: VIDA 2
    • Deep under for gold and biomarkers
    • Abu Dhabi sabkha and lagoon
    • Laguna Mendosa, Guatemala
    • Yellowstone Microbial films
    • Geological features at UIC
    • Geobiology Course 2015 - Luoth Chou
    • Just clouds and haloes
    • Flying over Greenland
    • Field trip to Missouri 2017
  • Facility
  • AN ORGANIC GEOCHEMISTRY PRIMER
    • A brief history of Organic Geochemistry
    • From bio- to geo-molecules
    • Diagenesis: Stereoisomerism
  • Contacts
Geological features at UIC. 

Our building, SES,  is dissolving slowly, resulting in the formation of stalagtites and stalagmites. 

The floor in SES is made of Minnesota Granite, note the basalt xenolith.  
 
Stalagmite and drapestone, SES
Stalagmite and drapestone, SES
Stalagmite, with pools
Pool, SES
Note the depressions left by dissolved fossils in the concrete
Stalagmite on the floor, SES
Inactive flowstone
Stalagtites
Stalagmite on Minnesota granite
Minnesota granite
Minnesota granite with basalt xenolith
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