Книга: Daly Reginald Aldworth «Igneous Rocks and Their Origin»

Igneous Rocks and Their Origin

Серия: "-"

Книга представляет собой репринтное издание. Несмотря на то, что была проведена серьезная работа по восстановлению первоначального качества издания, на некоторых страницах могут обнаружиться небольшие "огрехи" :помарки, кляксы и т. п.

Издательство: "Книга по Требованию" (2011)

Купить за 1318 руб в My-shop

Другие книги автора:

КнигаОписаниеГодЦенаТип книги
Origin of the iron ores at KirunaКнига представляет собой репринтное издание. Несмотря на то, что была проведена серьезная работа по… — Книга по Требованию, - Подробнее...2011411бумажная книга
The Differentiation of a Secondary Magma Trough Gravitative Adjustment, Volume 1Книга представляет собой репринтное издание. Несмотря на то, что была проведена серьезная работа по… — Книга по Требованию, - Подробнее...20111314бумажная книга
The Geology of Ascutney Mountain, VermontКнига представляет собой репринтное издание. Несмотря на то, что была проведена серьезная работа по… — Книга по Требованию, - Подробнее...2011680бумажная книга

Daly, Reginald Aldworth

▪ Canadian-American geologist
born May 19, 1871, Napanee, Ont., Can.
died Sept. 19, 1957, Cambridge, Mass., U.S.

      Canadian-American geologist who independently developed the theory of magmatic stoping, whereby molten magma rises through the Earth's crust and shatters, but does not melt, the surrounding rocks. The rocks, being denser than the magma, then sink, making room for the magma to rise. This theory was instrumental in explaining the structure of many igneous rock formations.

      In 1898 Daly was appointed geology instructor at Harvard University. In 1901 he became a geologist with the Canadian International Boundary Commission, and for six years he conducted surveys of the mountainous region of western Alberta and southern British Columbia. During this period, in 1903, he first proposed his theory of magmatic stoping.

      After he became professor of geology at Massachusetts Institute of Technology, Cambridge, in 1907, his travels took him to Hawaii and Samoa. From his studies of those islands came his theory of “glacial control” of the formation of coral atolls and reefs (coral reef). He found that the fluctuations of sea level during the building up and melting down of glaciers during the Pleistocene Epoch played a major role in allowing the coral to slowly build up structures more than 75 m (250 feet) high. He also proposed that submarine canyons were eroded by turbidity currents. In 1912 Daly became Sturgis Hooper Professor of Geology at Harvard University, retiring in 1942.

* * *

Источник: Daly, Reginald Aldworth

См. также в других словарях:

  • Ultrapotassic igneous rocks — are a class of rare, volumetrically minor generally ultramafic or mafic silica depleted igneous rocks. Ultrapotassic rocks are defined by molar K2O/Na2O >3 in much of the scientific literature. In other papers written as recently as 2005, they… …   Wikipedia

  • Igneous rock — Geologic provinces of the world (USGS)   Shield …   Wikipedia

  • igneous rock — Any of various crystalline or glassy, noncrystalline rocks formed by the cooling and solidification of molten earth material (magma). Igneous rocks comprise one of the three principal classes of rocks, the others being metamorphic and sedimentary …   Universalium

  • Large igneous province — Only a few of the largest Large Igneous Provinces are indicated (by the dark purple areas) on this geological map, which depicts crustal geologic provinces as seen in seismic refraction data. A Large Igneous Province (LIP) is an extremely large… …   Wikipedia

  • Earth and Space Sciences — ▪ 1996 Introduction GEOLOGY AND GEOCHEMISTRY       In 1995 significant developments took place in the realm of geologic mapping, which provides the foundation for the presentation and comparison of data in the Earth sciences. The most important… …   Universalium

  • Formation of rocks — This article discusses how rocks are formed. There are also articles on physical rock formations, also known as strata, and the formal naming of geologic formations. The three main ways rocks are formed: * Sedimentary rocks are formed through the …   Wikipedia

Поделиться ссылкой на выделенное

Прямая ссылка:
Нажмите правой клавишей мыши и выберите «Копировать ссылку»