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Geology of the Southern Part of Wellsville Mountain, Wasatch Range, UtahGelnett, Ronald H. 01 May 1958 (has links)
Wellsville Mountain is 10 miles west of Logan, Utah, at the northern extremity of the Wasatch Range. Paleozoic rocks forma northeast-dipping homocline bounded in part by northwest-trending high-angle faults and cut by a series of northeast-trending high-angle faults. A major transverse fault, with a stratigraphic displacement of 4,500 feet, divides the mountain into two distinct blocks.
The rock units of the area are comparable to those of the Logan quadrangle immediately to the east. Pre-Cambrian rocks crop out in Box Elder Canyon, just east of Brigham City, and are overlain by at least 20,000 feet of northeast-dipping Paleozoic rocks of every period except possibly the Permian. The Beirdneau sandstone member of the Jefferson formation, is tentatively correlated with that of the upper Devils Gate limestone of central Nevada. About 6,600 feet of the Oquirrh formation of Pennsylvanian age is exposed near the northern end of Wellsville Mountain. The presence of Desmoinesian fusulinids at the base of the Oquirrh and upper Virgilian fusulinids throughout the interval from 1,000 to 2,000 feet above its base indicates an absence of Lower Pennsylvanian rocks and suggests that the upper 4,400 feet may be in part Permian. Mesozoic rocks are not found in the area. The Wasatch formation and Salt Lake group of Tertiary age crop out in the foothills at the northern end of Wellsville Mountain.
Two fault systems are recognized in the area. The northeast-trending high-angle transverse faults of Laramide age and the north-west-trending high-angle bordering faults are Basin and Range age.
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Groot-Brittanje se aanspraak op die suidelike gedeelte van Delagoabaai, 1822 - 1875Edwards, Peter 25 November 2020 (has links)
Afrikaans: In die tydperk 1822 tot 1875 het Groot-Brittanje verskeie aansprake rakende
eienaarskap op die suidelike gedeelte van Delagoabaai gemaak wat tot ‘n aantal
insidente met Portugal gelei het. Hierdie aansprake het nie ‘n spesifieke patroon
gevolg nie.
Kaptein William Fitzwilliam Owen kan as die grondlegger van Britse aansprake op
die suidelike gedeelte van Delagoabaai beskou word. Sy ooreenkomste met die
inheemse leiers van Tembe en Maputo in 1823 het die grondslag vir Britse
aansprake op die suidelike gedeelte van Delagoabaai gelê.
Portugese protes teen Owen se aggressiewe bevordering van Britse belange in
Delagoabaai het reeds in 1826 tot die eerste korrespondensie op diplomatieke vlak
gelei. Hierdie korrespondensie, en veral die verskil in interpretasie oor die Anglo-
Portugese konvensie van 1817, sou in 1875 die grondslag van die Delagoabaaiarbitrasie
vorm.
Hernude Britse belangstelling in die handelsmoontlikhede van die suidelike gedeelte
van Delagoabaai het in November 1861 tot die Britse besetting van Inyackeiland in
die monding van die baai gelei. President M.W. Pretorius se poging in 1868 om die
Zuid-Afrikaansche Republiek se grondgebied tot Delagoabaai uit te brei en sy
daaropvolgende erkenning van Portugal se aanspraak op die suidelike gedeelte van
die baai, het protes van die Britse regering ontlok. Langdurige Anglo-Portugese
onderhandelinge het uiteindelik tot ‘n gesamentlike besluit gelei om hul opponerende
aansprake aan die arbitrasie van die Franse president, maarskalk Patrice
MacMahon, voor te lê. Op 27 Julie 1875 het MacMahon uitspraak ten gunste van
Portugal gelewer. / In the period of 1822 to 1875, Great Britain made various claims regarding
ownership of the southern part of Delagoa Bay which led to a number of incidents
with Portugal. These claims did not follow any specific pattern.
Captain William Fitzwilliam Owen can be regarded as the champion of the British
claim to the southern part of Delagoa Bay. His agreements with tribal leaders of
Tembe and Maputo in 1823 lay the foundation for the British claim to the southern
part of Delagoa Bay.
Portuguese protests against Owen’s aggressive advancement of British interests in
Delagoa Bay led to the first correspondence on diplomatic level in 1826. This
correspondence and especially the difference of interpretation of the Anglo-
Portuguese convention of 1817, would form the foundation of the Delagoa Bay
arbitration in 1875.
Renewed British interest in the possibility of trade relations with the southern part of
Delagoa Bay led to the British occupation of Inyack Island in the mouth of the Bay in
November 1861. The attempts of President M.W. Pretorius in 1868 to expand the
Zuid-Afrikaansche Republiek’sZ.A.R.’s territory to Delagoa Bay and his recognition
of Portugal’s claim to the southern part of the bay, led to protestation from the British
government. Lengthy Anglo-Portuguese negotiations would eventually lead to a
combined decision to have the issue of their opposing claims arbitrated by the
French president, Marshal Patrice MacMahon. On 27 July 1875 MacMahon decided
in favour of the Portuguese. / Thesis (PhD (Geskiedenis))--University of Pretoria, 2020. / Historical and Heritage Studies / PhD (Geskiedenis) / Unrestricted
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Studie náměstí v České Skalici / Study of the square in České SkaliceRejzek, Jan January 2019 (has links)
The aim of the diploma thesis is to design a suitable layout of the square in České Skalice. The work deals with the design of parking places, bus bays, barrier-free sidewalks and the design of pedestrian crossings and places for crossing. The other part is the layout of greenery and the improvement of the center of the square. In the framework of the work, three variants of the arrangement were elaborated. The most preferred option was further elaborated.
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