21,361 research outputs found
The Campbell clan in Virginia /
No full text"This book ... is based largely on the material in the book 'Some Campbell records,̓ published ... in 1942."Bibliography : p. v.Mode of access: Internet.SPECIAL COLLECTIONS: Gift of the author.2 1
Campbell autograph album, MSS.0265
No full textAbstract: An "Atlantic Cable Charm Book" autograph album owned by a person named Campbell, containing the signature of Sam Houston and various handwritten poems.Scope and Content Note: The collection contains one "Atlantic Cable Charm Book," an autograph album with the signature of Sam Houston and various handwritten poems. A letter inside the front cover by an unknown author tells Campbell that the album is a gift.Biographical/Historical Note: An unidentified person whose first name was Campbell owned this autograph album
Consistency determination, USCG Station Siuslaw : geotechnical borings
No full textprepared for: U.S. Coast Guard ; prepared by: Eric Campbell, Jodi Wilmoth, Campbell Environmental, LLC.This archived document is maintained by the State Library of Oregon. It is for informational purposes and may not be suitable for legal purposes.Includes bibliographical references.Mode of access: Internet from the State Library of Oregon U.S. Government Publications Collection.Text in English
Sarah C. Campbell & Richard, P. Campbell: Cook Prize 2023, Silver Medal Acceptance Speech.
No full textSarah Campbell (author & photographer) and Richard Campbell (photographer) give an acceptance speech and talk about their book Infinity: Figuring Out Forever. Published by Astra Young Readers.https://educate.bankstreet.edu/cook/1005/thumbnail.jp
Grim-Faced Ed Campbell
No full textPhotograph used for a story in the Daily Oklahoman newspaper. Caption: "GRIM-FACED ED CAMPBELL stands in front of the house he mistakenly built on property in for northeast Oklahoma City on Oklahoma County-owned land.
Sedimentary facies and unconformity analysis of some Paleocene-Eocene sections, Marlborough and Campbell Island, New Zealand
No full textThroughout the Late Cretaceous to Eocene, sedimentation in gradually subsiding basins on the passive eastern margin of the micro-continent of Zealandia recorded climatic and paleoceanographic changes in a greenhouse world. One such fundamental change in Southern Ocean circulation is hypothesised to be recorded in a regionally extensive unconformity surface and short-lived lithofacies changes contained within Late Paleocene to Early Eocene sedimentary successions at key sections throughout New Zealand, and investigated here on Campbell Island and in southeastern Marlborough.
On Campbell Island, this oceanographic event is represented by an unconformity between the Late Cretaceous to Late Paleocene Garden Cove Formation and the Early Eocene to Oligocene Tucker Cove Limestone. This unconformity signifies a major lithofacies change from Garden Cove Formation which consists of siliceous mudstone containing fine sand to coarse silt sized siliciclastic grains, pelletal glaucony grains and rare quartz pebbles, to a nannofossil and foraminiferal limestone containing little to no siliciclastic grains comprising the Tucker Cove Limestone. Geochemically this lithofacies change is characterised by a dramatic decrease in terrigenous supply and a shift from siliceous to calcareous productivity, along with a significant concentration of Zr and rare earth elements. Lithofacies at this site are inferred to record possible episodes of ice rafting and eventual unconformity formation by invigorated intermediate depth ocean currents which resulted in winnowing of seafloor sediments and concentration of heavy minerals.
At the distal Mead Stream site in southeastern Marlborough, deposition of bio-siliceous sediments of the Mead Hill Formation and Amuri Limestone was locally disrupted by deposition of the Waipawa Formation, the lateral equivalent of an important hydrocarbon source rock identified in several of New Zealand‟s sedimentary basins. In outcrop, the Waipawa Formation at Mead Stream is characterised by a very distinctive rusty‟ brown fissile appearance, while in thin section, though radiolarians and sponge spicules are common, the overall fine grained nature of the unit makes identification of other components difficult. Geochemical proxies show a significant increase in terrigenous supply in the Waipawa Formation, along with an increase in siliceous productivity concomitant with a decrease in oxygenation at the site. Lithofacies changes through the Late Paleocene at Mead Stream suggest the site lay under a zone of upwelling which resulted in an increase in siliceous productivity during the Late Paleocene.
At the more proximal sites of Muzzle Stream and Kaikoura wharf in southeastern Marlborough, Mead Hill Formation and Amuri Limestone are separated by an unconformity, overlain by Teredo Limestone. The Teredo Limestone is considered to be a lateral equivalent of the Waipawa Formation, but both the base and top of the Teredo Limestone are timetransgressive. This means that at Muzzle Stream the unit is contemporaneous with the Waipawa Formation (Late Paleocene), while at Kaikoura wharf the unit is entirely Early Eocene in age. At these sites, the Teredo Limestone Member of the Amuri Limestone is a calcareous greensand sometimes containing phosphatised limestone clasts and sharks teeth. In thin sections, the unit consists of well sorted, fine to very fine sand sized siliciclastic grains and fine sand sized pelletal and vermicular glaucony set in a calcareous matrix that shows evidence of secondary silicification. Unconformity formation and the subsequent deposition of the overlying Teredo Limestone record a period of invigorated intermediate depth ocean currents that resulted in the transport of siliciclastic grains and glaucony to these bathyal sites. This interpretation is supported by a palinspastic map of the Teredo Limestone that suggests the unit was deposited under different conditions than those responsible for the deposition of the bounding Mead Hill Formation and Amuri Limestone. This map also suggests the Teredo Limestone was deposited as a skin drift‟, here named the Clarence Drift, possibly under the influence of contour currents.
Based on similarities between unconformities and lithofacies changes in Late Paleocene to Early Eocene sedimentary sections and an earlier, well documented event at the Cretaceous/Tertiary boundary in southeastern Marlborough, evidence for a period of enhanced siliceous productivity, invigorated ocean currents and possible episodes of ice rafting is suggested to be consistent with a brief period of Antarctic ice sheet growth during a phase of global cooling in the Late Paleocene.
The possible identification of Antarctic ice sheets, ephemeral though they may have been, not only challenges long held beliefs that the Antarctic continent remained ice free during the early Paleogene greenhouse world but also questions the suggested mechanisms responsible for Antarctic ice sheet growth. The lack of ocean gateways in the Southern Ocean during this time effectively rules out thermal isolation of the Antarctic continent as a driver. Given that this period of ice sheet growth is contemporaneous with a documented period of enhanced global ocean productivity and terrestrial carbon accumulation and related draw down in atmospheric CO2, it is suggested this may represent the driver responsible for brief Antarctic glaciation during this period, though the postulated link requires further investigation
Charles Simeon Series: Dr. Con Campbell
No full textDr. Constantine Campbell preaches on 1 Peter about how to engage with culture without becoming like it, and how we are to see ourselves in relation to the world.
Dr. Constantine Campbell is Associate Professor of New Testament at Trinity Evangelical Divinity School. He is the author of several books on the Greek language and the Apostle Paul, including Paul and Union with Christ, which was the 2014 Christianity Today Book of the Year in Biblical Studies. Dr Campbell is a busy preacher, evangelist, author, and professionally trained jazz musician. He is married to Bronwyn with three kids, all of whom moved to the United States from their native Australia in 2013. Dr Campbell enjoys playing jazz saxophone, lifting weights, and playing chess, though not normally at the same time
NORAD: Building an educational network [video]
No full textIn this Viewpoints interview, Joint Education Officer Ed Campbell discusses the building relationship between academia and NORAD (The North American Aerospace Defense Command). Campbell, along with NORAD, has been contributing to the development of various research programs, online resources, and funding opportunities for students across the country. This interview exposes the various steps being taken towards the development of government-academic relationships, and emphasizes how these efforts will help make U.S. defense security programs more reliable and veritable
Letter from Carl Hayden to Hugh E. Campbell
No full textLetter from Carl Hayden to Hugh E. Campbell with an enclosed outline map of the proposed boundaries of Grand Canyon National Park
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