Francis P. Farquhar
Francis Peloubet Farquhar was an American mountaineer and author in addition to his career as a Certified Public Accountant. Farquhar was born in Newton, the son of David Webber Farquhar and Grace Thaxter Peloubet, he attended Harvard University, where he edited The Harvard Crimson for three years and studied under, among others, Bliss Perry and George Santayana. Graduating from Harvard in 1909, he came to San Francisco in 1910, where he worked for a publisher and began a lifelong interest in fine printing, he visited Yosemite and joined the Sierra Club in 1911. He returned to New England to pursue the profession of accounting, studying under Clinton Scovell, a pioneer in the field of cost accounting. In 1914 he moved again to California, he served in the Navy there and in Washington, D. C. during World War I. In 1922 he set up his own accounting firm in San Francisco. In 1936 he brought in Clifford Heimbuchder, who soon became a full partner in the firm, renamed Farquhar and Heimbucher. Farquhar was active in the Sierra Club, serving on its board of directors from 1924 to 1951 and president in 1933-1935 and 1948-1949.
He served as Sierra Club Bulletin editor from 1926 to 1946. Farquhar was a mountaineer who invited Robert L. M. Underhill to introduce proper use of modern Alpine rope techniques to Sierra Club members on an annual club High Trip in 1931, he made multiple first ascents. On August 26, 1921, he completed the first ascent of Middle Palisade by the south-west chute with Ansel Hall, he was the author of numerous articles for the Sierra Club and the California Historical Society, some of which were reprinted in book form. In 1956-59 he was editor of the American Alpine Journal published by the American Alpine Club, he wrote forewords for several books on California history. His best known book is History of the Sierra Nevada, still in print. In addition to serving as Sierra Club president, he was president of the California Society of Certified Public Accountants, California Academy of Sciences, the California Historical Society. In 1965 he was awarded the Sierra Club's John Muir Award for distinguished work as a conservationist and mountaineer.
He received the Henry R. Wagner Memorial Award of the California Historical Society in 1966; the University of California at Los Angeles conferred on him the honorary degree of Doctor of Humane Letters in 1967. In 1934 he married fellow mountaineer, his half brother was the Los Angeles architect Robert D. Farquhar, who moved in with the Farquhars in Berkeley in 1953. Marjorie Bridge Farquhar died in 1999 in San Francisco. Mount Farquhar, located 1.6 miles northwest of Mount Brewer in Kings Canyon National Park, was named in his honor. Since 1970, the Sierra Club has given the Francis P. Farquhar Mountaineering Award in his honor. 1925: Exploration of the Sierra Nevada, California Historical Society 1926: Place Names of the High Sierra, Sierra Club 1930: Up and Down California in 1860-1864: The Journal of William H. Brewer, University of California Press 1932: Joaquin Murieta, the Brigand Chief of California, Grabhorn Press, San Francisco 1938: Preface to Clarence King's The Helmet of Mambrino, The Book Club of California 1943: A Brief Chronology of Discovery in the Pacific Ocean from Balboa to Capt.
Cook's First Voyage, 1513 to 1770, Grabhorn Press, San Francisco 1947: Preface and editing, Clarence King's Mountaineering in the Sierra Nevada 1948: Yosemite, the Big Trees and the High Sierra: A Selective Bibliography, University of California Press, ISBN 978-1-57898-155-7 1950: Flight to the North Pole, 24 August 1949, Grabhorn Press 1953: First Ascents Throughout the World, 1901-1950, Grabhorn Press 1953: The Books of the Colorado River & the Grand Canyon, Fretwater Press, ISBN 978-1-892327-14-7 1957: Place Names for Bohemians: Clubhouse to Grove, Silverado Squatters 1959: Naming Alaska's mountains: with some accounts of their first ascents, American Alpine Club 1965: History of the Sierra Nevada, University of California Press, Berkeley, ISBN 0-520-01551-7 1968: "Comments on Some Bay Area Fine Printers" in Edwin Grabhorn: Recollections of the Grabhorn Press, University of California, Bancroft Library, Regional Oral History Office Francis Farquhar Obituary Francis P. Farquhar, Exploration of the Sierra Nevada Francis P. Farquhar, Place Names of the High Sierra Guide to the Francis P. Farquhar Papers at The Bancroft Library Portrait Photo on Mt. Whitney Francis P. Farquhar at Find a Grave
Sierra Peaks Section
The Sierra Peaks Section is a mountaineering society within the Angeles Chapter of the Sierra Club that serves to provide mountaineering activities for Sierra Club members in the Sierra Nevada, to honor mountaineers who have summited Sierra Nevada peaks. The Sierra Peaks Section was established in 1955; the Section maintains historic summit registers at Bancroft Library on the University of California, Berkeley campus. To become a member of the SPS, one must be a Sierra Club member and have climbed at least six peaks on the SPS List. For verification purposes, two of those ascents must be done on an official SPS trip. Accomplished members are award with emblems, with the following grades: Third List Completion Second List Completion First List Completion Master Emblem Senior Emblem EmblemUpon receiving one of the normal emblems, members may be recognized with one of the following additional emblems, which are not ranked: Geographic Emblem Explorer Emblem To the general public, they are most known for their peak bagging list, created in 1955, a product of the Sierra Club's long legacy of promoting climbing in the Sierra Nevada.
Completing the list is prestigious in American mountaineering circles, climbers who complete the list are cited as having done so. The list is divided into three levels of importance; the Emblem peaks are considered the most iconic peaks of the Sierra Nevada, to summit all of them is the goal of many peak baggers and alpinists. Mountaineers peaks are less notable peaks known for presenting mountaineering challenges. There are the numerous general peaks of lesser note; the list is an example of a subjective "decision by committee" list with the peaks on the list being determined by the Sierra Club. Peaks are added or removed from the list due to a variety of factors, such as accessibility and interest; the list is followed by thousands of hikers and has been noted in numerous books and guides on the Sierra Nevada. There are 15 Emblem peaks, 35 Mountaineers peaks, 197 general peaks, for a total of 247 peaks; the number of peaks is traditionally set at 248, the original number of peaks listed in 1955.
The elevations listed below are those described on the list, may not be the actual elevations of those peaks, although they are accurate to within 50 feet. Other peak bagging lists: New England Fifty Finest Adirondack High Peaks Secor, R. J.. The High Sierra: peaks, trail. Seattle, WA: Mountaineers Books. ISBN 978-0-89886-971-2. Official web site
The Cretaceous is a geologic period and system that spans 79 million years from the end of the Jurassic Period 145 million years ago to the beginning of the Paleogene Period 66 mya. It is the last period of the Mesozoic Era, the longest period of the Phanerozoic Eon; the Cretaceous Period is abbreviated K, for its German translation Kreide. The Cretaceous was a period with a warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas; these oceans and seas were populated with now-extinct marine reptiles and rudists, while dinosaurs continued to dominate on land. During this time, new groups of mammals and birds, as well as flowering plants, appeared; the Cretaceous ended with the Cretaceous–Paleogene extinction event, a large mass extinction in which many groups, including non-avian dinosaurs and large marine reptiles died out. The end of the Cretaceous is defined by the abrupt Cretaceous–Paleogene boundary, a geologic signature associated with the mass extinction which lies between the Mesozoic and Cenozoic eras.
The Cretaceous as a separate period was first defined by Belgian geologist Jean d'Omalius d'Halloy in 1822, using strata in the Paris Basin and named for the extensive beds of chalk, found in the upper Cretaceous of Western Europe. The name Cretaceous was derived from Latin creta; the Cretaceous is divided into Early and Late Cretaceous epochs, or Lower and Upper Cretaceous series. In older literature the Cretaceous is sometimes divided into three series: Neocomian and Senonian. A subdivision in eleven stages, all originating from European stratigraphy, is now used worldwide. In many parts of the world, alternative local subdivisions are still in use; as with other older geologic periods, the rock beds of the Cretaceous are well identified but the exact age of the system's base is uncertain by a few million years. No great extinction or burst of diversity separates the Cretaceous from the Jurassic. However, the top of the system is defined, being placed at an iridium-rich layer found worldwide, believed to be associated with the Chicxulub impact crater, with its boundaries circumscribing parts of the Yucatán Peninsula and into the Gulf of Mexico.
This layer has been dated at 66.043 Ma. A 140 Ma age for the Jurassic-Cretaceous boundary instead of the accepted 145 Ma was proposed in 2014 based on a stratigraphic study of Vaca Muerta Formation in Neuquén Basin, Argentina. Víctor Ramos, one of the authors of the study proposing the 140 Ma boundary age sees the study as a "first step" toward formally changing the age in the International Union of Geological Sciences. From youngest to oldest, the subdivisions of the Cretaceous period are: Late Cretaceous Maastrichtian – Campanian – Santonian – Coniacian – Turonian – Cenomanian – Early Cretaceous Albian – Aptian – Barremian – Hauterivian – Valanginian – Berriasian – The high sea level and warm climate of the Cretaceous meant large areas of the continents were covered by warm, shallow seas, providing habitat for many marine organisms; the Cretaceous was named for the extensive chalk deposits of this age in Europe, but in many parts of the world, the deposits from the Cretaceous are of marine limestone, a rock type, formed under warm, shallow marine circumstances.
Due to the high sea level, there was extensive space for such sedimentation. Because of the young age and great thickness of the system, Cretaceous rocks are evident in many areas worldwide. Chalk is a rock type characteristic for the Cretaceous, it consists of coccoliths, microscopically small calcite skeletons of coccolithophores, a type of algae that prospered in the Cretaceous seas. In northwestern Europe, chalk deposits from the Upper Cretaceous are characteristic for the Chalk Group, which forms the white cliffs of Dover on the south coast of England and similar cliffs on the French Normandian coast; the group is found in England, northern France, the low countries, northern Germany, Denmark and in the subsurface of the southern part of the North Sea. Chalk is not consolidated and the Chalk Group still consists of loose sediments in many places; the group has other limestones and arenites. Among the fossils it contains are sea urchins, belemnites and sea reptiles such as Mosasaurus. In southern Europe, the Cretaceous is a marine system consisting of competent limestone beds or incompetent marls.
Because the Alpine mountain chains did not yet exist in the Cretaceous, these deposits formed on the southern edge of the European continental shelf, at the margin of the Tethys Ocean. Stagnation of deep sea currents in middle Cretaceous times caused anoxic conditions in the sea water leaving the deposited organic matter undecomposed. Half the worlds petroleum reserves were laid down at this time in the anoxic conditions of what would become the Persian Gulf and the Gulf of Mexico. In many places around the world, dark anoxic shales were formed during this interval; these shales are an important source rock for oil and gas, for example in the subsurface of the North Sea. During th
A mountain range or hill range is a series of mountains or hills ranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form and alignment that have arisen from the same cause an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are found on many planetary mass objects in the Solar System and are a feature of most terrestrial planets. Mountain ranges are segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not have the same geologic structure or petrology, they may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, volcanic landforms resulting in a variety of rock types. Most geologically young mountain ranges on the Earth's land surface are associated with either the Pacific Ring of Fire or the Alpide Belt.
The Pacific Ring of Fire includes the Andes of South America, extends through the North American Cordillera along the Pacific Coast, the Aleutian Range, on through Kamchatka, Taiwan, the Philippines, Papua New Guinea, to New Zealand. The Andes is 7,000 kilometres long and is considered the world's longest mountain system; the Alpide belt includes Indonesia and Southeast Asia, through the Himalaya, Caucasus Mountains, Balkan Mountains fold mountain range, the Alps, ends in the Spanish mountains and the Atlas Mountains. The belt includes other European and Asian mountain ranges; the Himalayas contain the highest mountains in the world, including Mount Everest, 8,848 metres high and traverses the border between China and Nepal. Mountain ranges outside these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Great Dividing Range, the Altai Mountains and the Hijaz Mountains. If the definition of a mountain range is stretched to include underwater mountains the Ocean Ridges form the longest continuous mountain system on Earth, with a length of 65,000 kilometres.
The mountain systems of the earth are characterized by a tree structure, where mountain ranges can contain sub-ranges. The sub-range relationship is expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains. Equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, the White Mountains and the Blue Ridge Mountains are children of the Appalachians; the parent-child expression extends to the sub-ranges themselves: the Sandwich Range and the Presidential Range are children of the White Mountains, while the Presidential Range is parent to the Northern Presidential Range and Southern Presidential Range. The position of mountains influences climate, such as snow; when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the leeward side, it warms again and is drier, having been stripped of much of its moisture.
A rain shadow will affect the leeward side of a range. Mountain ranges are subjected to erosional forces which work to tear them down; the basins adjacent to an eroding mountain range are filled with sediments which are buried and turned into sedimentary rock. Erosion is at work while the mountains are being uplifted until the mountains are reduced to low hills and plains; the early Cenozoic uplift of the Rocky Mountains of Colorado provides an example. As the uplift was occurring some 10,000 feet of Mesozoic sedimentary strata were removed by erosion over the core of the mountain range and spread as sand and clays across the Great Plains to the east; this mass of rock was removed as the range was undergoing uplift. The removal of such a mass from the core of the range most caused further uplift as the region adjusted isostatically in response to the removed weight. Rivers are traditionally believed to be the principal cause of mountain range erosion, by cutting into bedrock and transporting sediment.
Computer simulation has shown that as mountain belts change from tectonically active to inactive, the rate of erosion drops because there are fewer abrasive particles in the water and fewer landslides. Mountains on other planets and natural satellites of the Solar System are isolated and formed by processes such as impacts, though there are examples of mountain ranges somewhat similar to those on Earth. Saturn's moon Titan and Pluto, in particular exhibit large mountain ranges in chains composed of ices rather than rock. Examples include the Mithrim Montes and Doom Mons on Titan, Tenzing Montes and Hillary Montes on Pluto; some terrestrial planets other than Earth exhibit rocky mountain ranges, such as Maxwell Montes on Venus taller than any on Earth and Tartarus Montes on Mars, Jupiter's moon Io has mountain ranges formed from tectonic processes including Boösaule Montes, Dorian Montes, Hi'iaka Montes and Euboea Montes. Peakbagger Ranges Home Page Bivouac.com
International Standard Book Number
The International Standard Book Number is a numeric commercial book identifier, intended to be unique. Publishers purchase ISBNs from an affiliate of the International ISBN Agency. An ISBN is assigned to each variation of a book. For example, an e-book, a paperback and a hardcover edition of the same book would each have a different ISBN; the ISBN is 13 digits long if assigned on or after 1 January 2007, 10 digits long if assigned before 2007. The method of assigning an ISBN is nation-based and varies from country to country depending on how large the publishing industry is within a country; the initial ISBN identification format was devised in 1967, based upon the 9-digit Standard Book Numbering created in 1966. The 10-digit ISBN format was developed by the International Organization for Standardization and was published in 1970 as international standard ISO 2108. Published books sometimes appear without an ISBN; the International ISBN agency sometimes assigns such books ISBNs on its own initiative.
Another identifier, the International Standard Serial Number, identifies periodical publications such as magazines and newspapers. The International Standard Music Number covers musical scores; the Standard Book Numbering code is a 9-digit commercial book identifier system created by Gordon Foster, Emeritus Professor of Statistics at Trinity College, for the booksellers and stationers WHSmith and others in 1965. The ISBN identification format was conceived in 1967 in the United Kingdom by David Whitaker and in 1968 in the United States by Emery Koltay; the 10-digit ISBN format was developed by the International Organization for Standardization and was published in 1970 as international standard ISO 2108. The United Kingdom continued to use the 9-digit SBN code until 1974. ISO has appointed the International ISBN Agency as the registration authority for ISBN worldwide and the ISBN Standard is developed under the control of ISO Technical Committee 46/Subcommittee 9 TC 46/SC 9; the ISO on-line facility only refers back to 1978.
An SBN may be converted to an ISBN by prefixing the digit "0". For example, the second edition of Mr. J. G. Reeder Returns, published by Hodder in 1965, has "SBN 340 01381 8" – 340 indicating the publisher, 01381 their serial number, 8 being the check digit; this can be converted to ISBN 0-340-01381-8. Since 1 January 2007, ISBNs have contained 13 digits, a format, compatible with "Bookland" European Article Number EAN-13s. An ISBN is assigned to each variation of a book. For example, an ebook, a paperback, a hardcover edition of the same book would each have a different ISBN; the ISBN is 13 digits long if assigned on or after 1 January 2007, 10 digits long if assigned before 2007. An International Standard Book Number consists of 4 parts or 5 parts: for a 13-digit ISBN, a prefix element – a GS1 prefix: so far 978 or 979 have been made available by GS1, the registration group element, the registrant element, the publication element, a checksum character or check digit. A 13-digit ISBN can be separated into its parts, when this is done it is customary to separate the parts with hyphens or spaces.
Separating the parts of a 10-digit ISBN is done with either hyphens or spaces. Figuring out how to separate a given ISBN is complicated, because most of the parts do not use a fixed number of digits. ISBN is most used among others special identifiers to describe references in Wikipedia and can help to find the same sources with different description in various language versions. ISBN issuance is country-specific, in that ISBNs are issued by the ISBN registration agency, responsible for that country or territory regardless of the publication language; the ranges of ISBNs assigned to any particular country are based on the publishing profile of the country concerned, so the ranges will vary depending on the number of books and the number and size of publishers that are active. Some ISBN registration agencies are based in national libraries or within ministries of culture and thus may receive direct funding from government to support their services. In other cases, the ISBN registration service is provided by organisations such as bibliographic data providers that are not government funded.
A full directory of ISBN agencies is available on the International ISBN Agency website. Partial listing: Australia: the commercial library services agency Thorpe-Bowker.