1000 resultados para East Orange


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Surficial sediments east of Dunnville, Ontario representing a limited deltaic/lacustrine/aeolian system are investigated with the aim of defining and interpreting their geological history by means of exarrrrning their sedimentology and interrelationships. The Folk and \oJard grain size statistics of samples fran the area were calculated. These sample parameters were e1en plotted on maps to detennine regional patterns. The strongest pattern observed was one of distinct fining to the east, away fran the sand source. Aeolian deposits were fourrl to be better sorted than the surrcunding sediments. The grain size parameter values were also plotted on bivariate graphs in an attempt to separate the samples according to depositional environment. This exercise met with little success, as rrost of the sediments sampled in the area have similar grain size parameters. This is believed to be because the sediment sources for the different environments (delta, distal delta, aeolian dune) are intimately related, to the point that nnst dunes appear to have been sourcErl fran immediately local sediments. It is FOstulated that in such a srrall sedimentological sub-system, sediments were not involved in active transport for a length of time sufficient for the rraterial to cane to equilibritnn with its transporting medium. Thus, fe..v distinctive patterns of parameters were developed that would enable one to differentiate between various environments of neposition. The i.rnTaturity of rrany dune forms and the i.Imaturity of mineralogical composition of all deposits support the above hyt:XJthesis of limited transport time. Another hypothesis proposen is that eadh geologically or geographically distinct area or "sub-system" rray have its o,.m "signature" of grain size relationships as plotted on bivariate graphs. Thus, the emphasis, concerning graphs of this type, should not be placErl on attempting to nifferentiate between various environnents of deposition, hut raB1er on investigating the interrelationships between sanples am environments within that "sub-system". Through the course of this investigation, the existence of nelta plain distributary Channels in the thesis area is SUG0ested, and the mscovery of significantly mfferent sub-units within the TUnnville dune sediments is documented. It is inferred by reference to other authors interpretations of the glacial history of the area, that the tirre of effective aeolian acti vi ty in the Dunnville area was between 12,300 to 12,100 years R.p.

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Aerial view of the Chapman College campus, Orange, California, 1966. Looking diagonally to the northeast. Corner of North Glassell Street and Palm Avenue in lower middle, with the five original buildings just beyond. The old gymnasium is by the oval playing field and stadium. Photographed by Rene Laursen, 702 N. Grand, Santa Ana, California [No. 1499#1].

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Aerial view of the Chapman College campus, Orange, California, February 23, 1973. Looking north; athletic field and stadium in center. Photographed by "Aerial Eye Inc. - Custom Aerial Photography - 1330 Bristol S. E. #103 - Santa Ana, California 92707." [#9]

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Aerial view of the Chapman College campus, Orange, California, February 23, 1973. North at left; athletic field and stadium in center. Photographed by "Aerial Eye Inc. - Custom Aerial Photography - 13

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Aerial view of the Chapman College campus, Orange, California, January, 1973. North at left; athletic field and stadium in center. Photographed by "Aerial Eye Inc. - Custom Aerial Photography - 1330 Palisades #92 - Santa Ana, California 92707." [#1]

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Aerial view of the Chapman College campus residence halls, Orange, California.

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Aerial view of the Chapman College campus, Orange, California. Looking northwest; the Moulton Fine Arts complex is at lower right. After 1978.

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Color postcard featuring an aerial view of the Chapman College campus, Orange, California, ca. 1995. Looking north. On message side: "Produced by Wayne Salvatti/Photografx; Copyright Photografx"

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Charles C. Chapman and Ethel Chapman Wickett at a birthday picnic for Charles C. Chapman at Orange County Park, California, July 2, 1937. [Copy an excerpt of CCCF27]

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Charles C. Chapman, Ethel Chapman Wickett and Stanley Chapman at birthday picnic for Charles C. Chapman at Orange County Park, California, July 2, 1937.

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Clara Irvin Chapman's last visit to the Chapman campus was in March, 1967 for the opening of the Thurmond Clarke Memorial Library. She is in the Heritage Room by a portrait of her late husband, Charles Clarke Chapman, for whom the college is named.

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Clara Irvin Chapman's last visit to the Chapman campus was in March, 1967 for the opening of the Thurmond Clarke Memorial Library. She is in the Heritage Room by a portrait of her late husband, Charles Clarke Chapman, for whom the college is named.

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Clara Irvin Chapman's last visit to the Chapman campus was in March, 1967 for the opening of the Thurmond Clarke Memorial Library. She is in the Heritage Room of the library.

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Chapman College Homecoming, Orange, California, 1978. Left to right: Irvin "Ernie" Chapman, Agnes Burghardt, and Edy Chapman.

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Chapman College Alumni Trustees pose for a portrait on the campus in Orange, California in the late 1980s. Left to right: James Roosevelt, A. Andrew Johnson, George Argyros, Harmon Wilkinson, Irvin C. Chapman and Myron Cole.