astronomy

Reginald Aldworth Daly

Reginald Aldworth Daly is a astronomy topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Reginald Aldworth Daly rather than just read about it. In short: Reginald Aldworth Daly (May 19, 1871 – September 19, 1957) was a Canadian geologist. He is best known for being one of the first proponents of the giant-impact hypothesis of the formation of the Moon.

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Reference excerpt

Reginald Aldworth Daly (May 19, 1871 – September 19, 1957) was a Canadian geologist. He is best known for being one of the first proponents of the giant-impact hypothesis of the formation of the Moon.

Biography Reginald Daly was educated at the University of Toronto, where geologist A.P. Coleman persuaded him away from teaching mathematics and into Earth Sciences. He obtained his PhD at Harvard, and did postgraduate work in Germany and France. After working as a field geologist for the International Boundary Commission, he was a professor, and headed the Department of Geology at Harvard University from 1912 until 1942. Daly was president of The Geological Society of America in 1932. For the Boundary Commission, working in six field seasons, Daly mapped the border from the Pacific Ocean to the Great Plains, a rugged swath 400 miles (640 km) long and 5 to 10 miles (8.0 to 16.1 km) wide – an area of about 2,500 square miles (6,500 km2). He documented the geology alone, but had the help of one field assistant and numerous wranglers and porters. He collected 1,500 rock specimens and made 960 thin sections, using a German polishing technique he learnt as a student. The project also included 1,300 photographs, dozens of lake soundings, stratigraphic and structural mapping, petrology, and morphology. In 1912, he filed his final report with the Geological Survey of Canada, a massive 3-volume tome he called North America Cordillera: Forty-Ninth Parallel. This work along the 49th parallel led him to formulate a theory of the origins of igneous rocks, and later publish his seminal work Igneous Rocks and Their Origin in 1914. According to Daly's biographer, James Natland, Daly was an early proponent of Arthur Holmes and Alfred Wegener's continental drift theory. Daly summarized his ideas in his 1926 book, Our Mobile Earth, which included on the title page small print adopted from Galileo: E pur si muove. Daly's theory on continental displacement was based partly on the idea that after the Moon was ejected from the Earth, continental movement was an inevitable part of rebalancing the planet; he also suggested that continental material accruing near oceans eventually slips, and forces continents to creep along. He expanded this notion in Strength and Structure of the Earth, in 1940, where Daly anticipated aspects of plate tectonics, including introduction of a "mesospheric shell" and a slippery vitreous basaltic substratum. Daly also proposed the impact theory of lunar creation in 1946, which countered two prevailing notions: George Darwin's hypothesis that the Moon spun out of the primordial Earth due to centrifugal force; and, another fashionable theory that the Moon was a captured wayward asteroid. Daly applied Newtonian physics to make his point, which was later validated. His doctoral students included the Canadian geologist Norman L. Bowen, who, based on experiments and observations of natural rocks, summarized the order of crystallization of common silicate minerals from typical basaltic magma undergoing fractional crystallization, now known as Bowen's reaction series.

Family In 1903, Daly married Louise Porter Haskell, daughter of Alexander Cheves Haskell and Alice Van Yeveren, and elder sister of Mary Elizabeth Haskell. After their marriage, Louise accompanied Daly on his travels, and in the field, as an assistant. She did much of the work in preparing and editing his manuscripts and books, and Daly's 1914 book on 'Igneous Rocks and their Origin' is dedicated to her; his "inspiring fellow worker".

Awards In 1909, Daly was elected a member of the American Academy of Arts and Sciences. He was elected to the American Philosophical Society in 1913 and the United States National Academy of Sciences in 1925. Daly was awarded the Penrose Medal in 1935, the Wollaston Medal in 1942 and the William Bowie Medal in 1946. In 1950 he became foreign member of the Royal Netherlands Academy of Arts and Sciences. The potassium zirconium silicate mineral dalyite and craters on Mars and the Moon are named in his honor. His Cambridge, Massachusetts, house (the Reginald A. Daly House) is now a National Historic Landmark.

References

Bibliography Daly, R A (1940), "Strength and Structure of the Earth", Prentice-Hall, New York, p. 434, hdl:2027/mdp.39015005801728, ISBN 978-0028435206 {{citation}}: ISBN / Date incompatibility (help) Daly, RA (1933), "The Depths of the Earth", Science, 77 (1987) (published Jan 27, 1933): 95–102, Bibcode:1933Sci....77...95D, doi:10.1126/science.77.1987.95, PMID 17797838 Daly, RA (1931), "Gardiner on Coral Reefs", Science, 74 (1927) (published Dec 4, 1931): 566–567, Bibcode:1931Sci....74..566D, doi:10.1126/science.74.1927.566, PMID 17807633 Daly, R A (1920), "A General Sinking of Sea-Level in Recent Time", Proc. Natl. Acad. Sci. U.S.A., vol. 6, no. 5 (published May 1920), pp. 246–50, Bibcode:1920PNAS....6..246D, doi:10.1073/pnas.6.5.246, PMC 1084496, PMID 16586806 Daly, R A (1917), "Low-Temperature Formation of Alkaline Feldspars in Limestones", Proc. Natl. Acad. Sci. U.S.A., vol. 3, no. 11 (published Nov 1917), pp. 659–65, Bibcode:1917PNAS....3..659D, doi:10.1073/pnas.3.11.659, PMC 1091350, PMID 16576265 Daly, R A (1916), "A New Test of the Subsidence Theory of Coral Reefs", Proc. Natl. Acad. Sci. U.S.A., vol. 2, no. 12 (published Dec 1916), pp. 664–70, Bibcode:1916PNAS....2..664D, doi:10.1073/pnas.2.12.664, PMC 1091132, PMID 16586654 Daly, RA (1901), "Notes on Oceanography", Science, vol. 13, no. 337 (published Jun 14, 1901), pp. 951–954, Bibcode:1901Sci....13..951D, doi:10.1126/science.13.337.951, PMID 17733661 Daly, RA (1901), "Scientific Expedition to Iceland, Greenland and Labrador", Science, 13 (318) (published Feb 1, 1901): 192, Bibcode:1901Sci....13R.192D, doi:10.1126/science.13.318.192, PMID 17816318

Further reading Mather, Kirtley (1970–1980). "Daly, Reginald Aldworth". Dictionary of Scientific Biography. Vol. 3. New York: Charles Scribner's Sons. pp. 547–548. ISBN 978-0-684-10114-9. Robert M. Hazen: Reginald Aldworth Daly (1871-1957). Archived 2009-05-24 at the Wayback Machine Daly's Biography, American Geophysical Union James H. Natland: Reginald Aldworth Daly (1871–1957): Eclectic Theoretician of the Earth. GSA Today, vol. 16, no. 2, 2006 Francis Birch: Reginald Aldworth Daly, 1871-1957, A Biographical Memoir National Academy of Sciences, Washington, DC, 36 pp., 1960

External links Works by or about Reginald Aldworth Daly at the Internet Archive

Worked examples

Example 1 — a first encounter with Reginald Aldworth Daly

Start with the simplest possible case. Write down what Reginald Aldworth Daly claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In astronomy, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Reginald Aldworth Daly before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Reginald Aldworth Daly ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Reginald Aldworth Daly

In research: Reginald Aldworth Daly appears in astronomy research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry: Engineering practice reuses Reginald Aldworth Daly in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom: Reginald Aldworth Daly is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1871 births, 1957 deaths, Canadian geologists, so understanding it makes those chapters shorter.
In everyday life: Look for Reginald Aldworth Daly outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

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Frequently asked questions

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