Книга: Conybeare William Daniel «An analytical examination into the character, value, and just application of the writings of the Christian fathers during the ante-Nicene period. Being the Bampton lectures for the year MDCCCXXXIX»
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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)
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Conybeare, William Daniel
▪ British geologist
born June 7, 1787, St. Botolph, West Sussex, Eng.
died Aug. 12, 1857, Itchen Stoke
English geologist and paleontologist, known for his classic work on the stratigraphy of the Carboniferous (280,000,000 to 345,000,000 years ago) System in England and Wales.
Conybeare was vicar of Axminster from 1836 until 1844, when he became dean of Llandaff, in Wales. In 1822 he and William Phillips produced their classic Outlines of the Geology of England and Wales (1822), in which fossils were used to date sedimentary formations; the book summarized geologic layers of Great Britain to the Carboniferous.
Conybeare contributed to the elucidation of the geology of Ireland and was also one of the first to use geologic cross sections to express subsurface structure. He wrote On the Origin of a Remarkable Class of Organic Impressions Occurring in Nodules of Flint (1814), Hydrographical Basin of the Thames (1829), and Ichthyosaurus (1821), the first description of this animal.
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Источник: Conybeare, William Daniel
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| Автор | Книга | Описание | Год | Цена | Тип книги |
|---|---|---|---|---|---|
| Conybeare William Daniel | An analytical examination into the character, value, and just application of the writings of the Christian fathers during the ante-Nicene period. Being the Bampton lectures for the year MDCCCXXXIX | Книга представляет собой репринтное издание. Несмотря на то, что была проведена серьезная работа по… — Книга по Требованию, - Подробнее... | 2011 | 1322 | бумажная книга |
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