Frank Fitch Grout

Frank Fitch Grout (January 24, 1880, Rockford, Illinois – August 1, 1958, Minneapolis) was an American petrographer, geologist, and mineralogist. He is perhaps best known for introducing the term lopolith into the science of geology. The mineral groutite is named in Grout's honor (based upon a 1945 discovery by John Walter Gruner).

Biography
Grout graduated from the high school course offered at Throop Polytechnic Institute and Manual Training School and then briefly studied at Throop College (precursor to Caltech), before transferring to the University of Minnesota. There he graduated with a bachelor's degree in chemistry in 1904. He was employed in 1905 by the West Virginia Geological Survey and in 1906 by the Illinois Geological Survey. He was briefly employed as an instructor by the University of Oklahoma. At the University of Minnesota, he joined in 1907 the academic staff of the geology department and retained academic appointments there until his retirement. He was promoted to full professor in 1919 and retired in 1948 as professor emeritus. He received in 1908 a master's degree in geology from the University of Minnesota and in 1917 a Ph.D. in geology from Yale University. His Ph.D. thesis deals with pegmatites of the Duluth gabbro. In December 1947 he gave an address to a conference sponsored by the Geological Society of America. Grout gained an outstanding reputation as a teacher. In retirement, he taught successively at several universities: Florida State}, Columbia, Arizona, and Caltech.

For about 35 years from 1919 to 1944, Grout spent most of his summers doing supervisory fieldwork for the Minnesota Geological Survey. This supervisory role was delegated to him by William Harvey Emmons (1876–1948). (Emmons was from 1911 to 1944 the head of the University of Minnesota's geology and, simultaneously, the director of the Minnesota Geological Survey.) Grout was extremely productive during these summers and completed, with his junior colleagues, many valuable reports. Grout enjoyed this summer fieldwork in the lake country of Minnesota and adjacent area in Ontario. In the lake country, he and his colleagues travelled by canoe and portage and camped in rarely visited areas. When he died his ashes were scattered on Saganaga Lake, on whose shores he had done geological research.

Grout was primarily a petrologist and petrographer, but he also did research on "clays, coal, iron formation and ores, mineralogy, chemical analysis of rocks and Precambrian stratigraphy." He was particularly interested in the geology of the Duluth Complex. Concerning the Duluth Complex, there was a controversy between Norman L. Bowen, on one side, and R. A. Daly and F. F. Grout, on the other side, about the role of differentiation processes in magmas. The Duluth Complex consists of two layers, a thicker lower layer essentially gabbro and an upper red layer that more closely resembles granite (called granophyre). There is no major transition in between, as would have been expected under Bowen's theory of differentiation/crystallization. Grout pointed out evidence of convection in the magma.

In July 1906 in Minneapolis, Frank F. Grout married May W. Browne. Upon his death in 1958, he was survived by his widow, their daughter, and four grandchildren.