ÿþ<HTML xmlns:v="urn:schemas-microsoft-com:vml" xmlns:o="urn:schemas-microsoft-com:office:office" xmlns:w="urn:schemas-microsoft-com:office:word" xmlns="http://www.w3.org/TR/REC-html40"> <HEAD> <meta name=Title content="Oldoinyo Lengai, East African Rift"> <meta name=Keywords content=""> <meta http-equiv=Content-Type content="text/html; charset=macintosh"> <meta name=ProgId content=Word.Document> <meta name=Generator content="Microsoft Word 10"> <meta name=Originator content="Microsoft Word 10"> <link rel=File-List href="lengai_files/filelist.xml"> <link rel=Edit-Time-Data href="lengai_files/editdata.mso"> <TITLE>Oldoinyo Lengai research</TITLE> <LINK REL="stylesheet" TYPE="text/css" HREF="stylesheet.css"> </HEAD> <BODY BACKGROUND="smoke1.jpg" BGCOLOR="silver" LANG="EN-US" LEFTMARGIN="60"> <BR> <H1>Oldoinyo Lengai, East African Rift</H1> <H2>World's only active carbonatite volcano</H2> <HR WIDTH="60%"> <BR> <P>I had the opportunity to join a French expedition organized by scientists from Le Centre National de la Recherche Scientifique (CNRS) to sample volatiles discharging from Oldoinyo Lengai, Tanzania. We had spent three days in the crater and then the volcano started erupting. This allowed us to not only sample pristine mantle volatiles but also fresh carbonatite lavas.</P> <BR> <IMG SRC="lengai_files/lengai1.jpg" WIDTH="382 HEIGHT="286" BORDER="3"> <BR>Oldoinyo Lengai lava flow, about two days old. <BR><BR><BR> <IMG SRC="lengai_files/lengai2.jpg" WIDTH="382" HEIGHT="287" BORDER="3"> <BR>Sampling of active flow (B. Marty and T. Fischer) <BR><BR> <H3>Publications from this work:</H3> <P CLASS="reference"><B>Fischer, T.P.</B>, Burnard, P., Marty, B., Hilton, D.R., Furi, E., Palhol, F., Sharp, Z.D., and Mangasini, F. (2009) Upper-mantle volatile chemistry at Oldoinyo Lengai volcano and the origin of carbonatites, Nature, 459, 77-80 doi:10.1038/nature07977 </BODY> </HTML>