Rockefeller Chapel is a Gothic Revival chapel on the campus of the University of Chicago in Chicago, Illinois. A monumental example of Collegiate Gothic architecture, it was meant by patron John D. Rockefeller to be the "central and dominant feature" of the campus; at 200.7 feet[1] it is by covenant the tallest building on campus.
Contents
1Design
2Carillon
3References
4External links
Design
Designed by architect Bertram Goodhue between 1918 and 1924, and built between 1925 and 1928 without the use of structural steel, it contains about 70 integrated figural sculptures by sculptors Lee Lawrie and Ulric Ellerhusen, and interior work by mosaicist Hildreth Meiere. Today the chapel is used for ecumenical worship services, weddings, university convocations, guest speakers, musical programs, and occasional film screenings. It occupies most of a block and can seat 1700 people.
The woodcarvings that adorn the organ and South balcony were created by Alois Lang, a Master Woodcarver at the American Seating Co., and one of the artists responsible for bringing the medieval art of ecclesiastical carving back to life. His pieces in Rockefeller Chapel are carved from White Appalachian Oak.
Carillon
The chapel contains the Laura Spelman Rockefeller Memorial Carillon and tower, a separate gift from John D. Rockefeller, Jr. in 1932 in honor of his mother. This 72-bell carillon is the second-largest carillon in the world by mass, after the carillon at Riverside Church on the Upper West Side of New York City, which Rockefeller Jr. also donated in honor of his mother.
Clash Royale CLAN TAG #URR8PPP A coarse-grained mafic intrusive rock Gabbro Photomicrograph of a thin section of gabbro Gabbro ( / ˈ ɡ æ b r oʊ / ) is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is chemically equivalent to rapid-cooling, fine-grained basalt. Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism. Due to its variant nature, the term "gabbro" may be applied loosely to a wide range of intrusive rocks, many of which are merely "gabbroic". Contents 1 Etymology 2 Petrology 3 Distribution 4 Uses 5 See also 6 References 7 External links Etymology The term "gabbro" was used in the 1760s to name a set of rock types that were found in the ophiolites of the Apenn
Clash Royale CLAN TAG#URR8PPP 
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