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Relevant bibliographies by topics / Paleobotany – Yukon – Klondike River Valley

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Dissertations / Theses
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Academic literature on the topic 'Paleobotany – Yukon – Klondike River Valley'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 February 2022

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Journal articles on the topic "Paleobotany – Yukon – Klondike River Valley"

1

Fraser, T. A., and C. R. Burn. "On the nature and origin of "muck" deposits in the Klondike area, Yukon Territory." Canadian Journal of Earth Sciences 34, no. 10 (1997): 1333–44. http://dx.doi.org/10.1139/e17-106.

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Organic-rich "muck" deposits, which blanket auriferous gravels in the Klondike area, Yukon Territory, comprise two principal stratigraphic units: (i) a silty Late Pleistocene deposit, and (ii) Holocene organics lying unconformably on the silt. The deposits are found predominantly in valley bottoms and, if undisturbed, are normally perennially frozen. Field and laboratory investigations of particle size, mineralogy, and morphology, as well as organic matter and sedimentary structures, indicate that the silt is both primary (massive) and redeposited (bedded) loess (by weight 87% medium and coars

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2

Kojima, S. "Ecosystem types of boreal forest in the North Klondike River Valley, Yukon Territory, Canada, and their productivity potentials." Environmental Monitoring and Assessment 39, no. 1-3 (1996): 265–81. http://dx.doi.org/10.1007/bf00396149.

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3

Barendregt, René W., Randolph J. Enkin, Alejandra Duk-Rodkin, and Judith Baker. "Paleomagnetic evidence for multiple late Cenozoic glaciations in the Tintina Trench, west-central Yukon, CanadaThis article is a companion paper to Duk-Rodkin et al., also in this issue." Canadian Journal of Earth Sciences 47, no. 7 (2010): 987–1002. http://dx.doi.org/10.1139/e10-021.

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The Tintina Trench in west-central Yukon has preserved an extensive record of late Cenozoic preglacial, glacial, and interglacial deposits. These deposits comprise multiple sequences of tills, outwash, loesses, and paleosols. The sediments that were laid down directly by ice (tills) are of both local (montane) and regional (Cordilleran) provenance. The Tintina Trench area was impacted repeatedly by montane ice from the southern Ogilvie Mountains to the northwest (2500 m above sea level (asl)), and also repeatedly along its southern extent by Cordilleran ice from the Selwyn Mountains to the eas

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Dissertations / Theses on the topic "Paleobotany – Yukon – Klondike River Valley"

1

Morse, Kathryn Taylor. "The nature of gold : an environmental history of the Alaska/Yukon gold rush /." Thesis, Connect to this title online; UW restricted, 1997. http://hdl.handle.net/1773/10468.

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Bornstein, Sara. "Women of the 1898 Alaska-Klondike Gold Rush." Diss., Connect to the thesis, 2009. http://hdl.handle.net/10066/3588.

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3

Lapp, Anthony. "Seasonal Variability of Groundwater Contribution to Watershed Discharge in Discontinuous Permafrost in the North Klondike River Valley, Yukon." Thesis, Université d'Ottawa / University of Ottawa, 2015. http://hdl.handle.net/10393/32298.

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The objectives of this thesis were: (1) to quantify seasonal groundwater contribution to total stream discharge and (2) further our understanding of sub-arctic carbon sources and pathways within a sub-arctic discontinuous permafrost river catchment. Twenty-two samples were taken from the North Klondike River, 14 samples from 5 of its tributaries, and 46 rain and snowmelt samples from the Dawson City Airport, Yukon, Canada,. During the winter months, groundwater is responsible for greater than 95% of total river discharge. Spring freshet and summer flow bring snowmelt and precipitation, cont

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4

MacKenzie, Douglas James, and n/a. "Structural controls on orogenic gold mineralisation in the Otago Schist, New Zealand and the Klondike Schist, Canada." University of Otago. Department of Geology, 2008. http://adt.otago.ac.nz./public/adt-NZDU20080704.085108.

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Orogenic gold mineralisation in schist terranes with few or no contemporaneous igneous intrusions is poorly understood. It is proposed in this thesis that the structural evolution of such terranes controls the generation of hydrothermal fluid pathways and thus the location of orogenic mineral deposits. Gold mineralisation in the Otago Schist, New Zealand and the Klondike Schist, Canada occurred in the latter phases of greenschist facies metamorphism as well as after metamorphism during Paleozoic-Mesozoic exhumation. In Otago, gold mineralisation occurred at a number of different times and stru

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5

Beyreis, David Charles. "Middle-class masculinity and the Klondike gold rush." 2007. http://digital.library.okstate.edu/etd/umi-okstate-2232.pdf.

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Books on the topic "Paleobotany – Yukon – Klondike River Valley"

1

Adney, Edwin Tappan. The Klondike stampede. UBC Press, 1994.

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2

The Klondike fever: The life and death of the last great gold rush. 2nd ed. Carroll & Graf, 2004.

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3

Candy, Waugaman, ed. A Klondike centennial scrapbook: Movies, music, guides, photographs, artifacts, and personalities of the great Klondike gold rush. Pictorial Histories Pub. Co., 1996.

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4

Berton, Pierre. Stampede for gold: The story of the Klondike Rush. Sterling Pub. Co., 2007.

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5

Good time girls of the Alaska-Yukon gold rush. Whitecap Books, 1999.

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6

Morgan, Lael. Good time girls of the Alaska-Yukon gold rush. Epicenter Press, 1998.

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7

Cushman, Dan. In Alaska with Shipwreck Kelly. Thorndike Press, 1997.

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8

In Alaska with Shipwreck Kelly: A north-western story. Five Star Western, 1996.

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9

Murphy, Claire Rudolf. Gold rush women. Hillside Press, 2012.

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10

Murphy, Claire Rudolf. Gold rush women. Alaska Northwest Books, 1997.

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Book chapters on the topic "Paleobotany – Yukon – Klondike River Valley"

1

Kojima, S. "Ecosystem Types of Boreal Forest in the North Klondike River Valley, Yukon Territory, Canada, and Their Productivity Potentials." In Global to Local: Ecological Land Classification. Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-1653-1_20.

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