Composition of sedimentary rocks from the Shapkina River valley, Bolshezemelskaya Tundra

A facies-genetic and stratigraphic subdivision of the Quaternary sequence in the Shapkina River valley has been accomplished. The riverbank shows outcrops of three glacial complexes with different mineralogical-petrographic compositions and structural characteristics, which can be correlated and stratificated. Datings of intermoraine horizons (alluvial, marine, lacustrine, and lacustrine-boggy sediments) have been based on palynological and paleomicrotheriological data. The Middle Neopleistocene section can be divided into two till horizons corresponding to two autonomous glaciations (Pechora and Vychegda). They are separated by a member of subaqueous Rodionov sediments. The Pechora till formed in the course of glacier motions from the northeast. Glacial horizons are mainly composed of the Vychegda till transported from the Northwest terrigenous provenance. Lithology of the Upper Neopleistocene Polyarnyi till testifies to its formation in the upper course of the river from material transported from the Northeast terrigenous-mineralogical provenance in the upper course of the river and from the Fennoscandian glaciation center in the lower course of the river. The paper presents the first lithological investigation and substantiation of genesis of various facies of Neopleistocene intermoraine marine sediments (sediments of the beach and fore-beach zones and shallow-water shelf).

University of Michigan Men's Tennis Team, 1985

Back Row: head coach Brian Eisner, Bradley Koontz, Jon Morris, Thomas Anderson, John Royer, Jed Hakken, Ed Filer, assistant coach Mark Mees

Front Row: Hugh Kwok, Jim Sharton, Chris Colwell, Franz Geiger, Kurt Lichtman, John Solik

University of Michigan Men's Tennis Team, 1986

Front Row: John Solik, Franz Geiger, Hugh Kwok, Jim Sharton, Chip McColl, Mike Pizzutello, Chris Colwell

Back Row: assistant coach Mark Mees, Ed Filer, Jed Hakken, Jon Morris, John Royer, Dan Goldberg, Brad Koontz, head coach Brian Eisner

The Royal Acquantainces of Memi and Sabu

Sculpture, Egyptian, Old Kingdom; 2 ft. 13/32 in.x 9 41/64 in.x 5 63/64 in.; painted limestone

Group of Two Women and a Child

Sculpture, Egyptian, Middle Kingdom to early New Kingdom; 2 51/64 in.x 1 11/16 in.x 3 15/64 in.; painted limestone

Tomb of Amenhotep, excavated artifact, Yuni and His Wife Renenutet, front view

Asyut, Egypt; 2 ft. 9 17/64 in.x 1 ft. 9 29/64 in.x 2 ft. 4 47/64 in.; painted limestone

Tomb of Amenhotep, excavated artifact, Yuni and His Wife Renenutet, rear view, two scenes illustrating the ancient Egyptian ideal of affection and remembrance among family generations

Asyut, Egypt; painted limestone

Statue of Kedamun and His Family

Sculpture, Egyptian, New Kingdom; 11 13/16 in.x 7 9/32 in.x 8 5/64 in.; painted limestone

Statue of Kedamun and His Family

Sculpture, Egyptian, New Kingdom; 11 13/16 in.x 7 9/32 in.x 8 5/64 in.; painted limestone

Fragments Depicting a Court Scene

Sculpture, Egyptian, New Kingdom; 8 15/32 in.x 1 ft. 9 1/16 in.; painted limestone

Preliminary report on a uranium occurrence in the Atlanta area, Lincoln County, Nevada /

Surface and airborne prospecting of the Ely Springs dolomite is recommended in this region, especially near silicified breccia pipes.

Mémoires de l'Académie des sciences, arts et belles-lettres de Dijon.

Some vols. issued with separate section title pages: Partie des lettres, Partie des sciences, etc.

Year-book for 1907.

Director: H. Foster Bain.

Royal Cemetery, PG779, excavated artifact, #U.11164, Standard of Ur, both sides

Ur (deserted settlement), Iraq; shell, lapis lazuli, red limestone; set in bitumen

Royal Cemetery, PG779, excavated artifact, #U.11164, Standard of Ur, front, War side

Ur (deserted settlement), Iraq; 8 1/2 in. x 1 ft. 7 1/2 in8 1/2 in. x 1 ft. 7 1/2 in.; shell, lapis lazuli, red limestone; set in bitumen