Academic literature on the topic 'Bandelier National Monument'

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Journal articles on the topic "Bandelier National Monument"

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Ramenofsky, Ann F. "The Historic Period at Bandelier National Monument. Monica L. Smith." Journal of Anthropological Research 60, no. 1 (April 2004): 124–26. http://dx.doi.org/10.1086/jar.60.1.3631017.

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DODD, DOUGLAS W. "Bandelier National Monument. National Park Service. Los Alamos, New Mexico. DARLENE KOONTZ, superintendent." Public Historian 29, no. 4 (2007): 124–28. http://dx.doi.org/10.1525/tph.2007.29.4.124.

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Creamer, Winifred. "Archaeology of Bandelier National Monument: Village Formation on the Pajarito Plateau. Timothy Kohler." Journal of Anthropological Research 60, no. 4 (December 2004): 617–20. http://dx.doi.org/10.1086/jar.60.4.3631171.

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Ellison, Laura E., A. Lance Everette, and Michael A. Bogan. "EXAMINING PATTERNS OF BAT ACTIVITY IN BANDELIER NATIONAL MONUMENT, NEW MEXICO, BY USING WALKING POINT TRANSECTS." Southwestern Naturalist 50, no. 2 (June 2005): 197–208. http://dx.doi.org/10.1894/0038-4909(2005)050[0197:epobai]2.0.co;2.

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Reneau, Steven L. "Stream incision and terrace development in Frijoles Canyon, Bandelier National Monument, New Mexico, and the influence of lithology and climate." Geomorphology 32, no. 1-2 (February 2000): 171–93. http://dx.doi.org/10.1016/s0169-555x(99)00094-x.

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Porter, Douglas, David Broxton, Angelyn Bass, Deborah A. Neher, Thomas R. Weicht, Patrick Longmire, Michael Spilde, and Rebecca Domingue. "The Role of Case Hardening in the Preservation of the Cavates and Petroglyphs of Bandelier." MRS Advances 2, no. 37-38 (2017): 1969–2005. http://dx.doi.org/10.1557/adv.2017.277.

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ABSTRACTBandelier National Monument (BNM) was created to protect an extraordinary inventory of archaeological resources carved in the Tshirege Member of the Bandelier Tuff. These include more than one thousand excavated chambers, called cavates, used for dwelling, storage, and textile production. The glass-rich tuffs at the base of the Tshirege Member are poorly consolidated and susceptible to erosion by wind, rain, and mechanical abrasion, with resultant loss of cultural material. However, rock surfaces develop protective weathering rinds that are resistant to erosion. Using optical microscopy, SEM-EDS, XRD, and electron microprobe analysis, we determined that this rind consists of clay and silt sediments colonized by lichens and other surface biota, accompanied by the precipitation of secondary minerals in the near-surface pore space. Scoping experiments focused on glass-organic acid interactions indicate that oxalic acid excreted by microbial crust constituents catalyzes biogeochemical reactions that lead to the preferential dissolution of Si, Al, and Fe components of the volcanic glass; these cations become available for precipitation of opal, and smectite and sepiolite clays. Enzyme assays that quantify biological activity at outcrop surfaces indicate that microbial populations initially thrive as they derive nutrients from the dissolution reactions of the glass, but activity starts to decline as precipitation of secondary minerals limits access to new sources of nutrients, so that alteration processes are self-limiting. As case hardening progresses, imbibition rates at the surface decrease, and the erosion resistance of the altered surfaces is substantially improved. This article presents summary results of research conducted over a period of five years to characterize the roles of lichens and other microflora in rind formation, and the resulting contributions to tuff stability. The interaction of lichens and other microflora with rock surfaces in archaeological sites and monuments is usually explored in terms of biodeterioration and consequent damage. However, this study shows that, under some circumstances, lichens and microflora provide a level of erosion protection to relatively porous and unconsolidated rock strata that outweighs their biodeteriorative effects.
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Barclay, Angela D., Julio L. Betancourt, and Craig D. Allen. "Effects of seeding ryegrass (Lolium multiflorum) on vegetation recovery following fire in a ponderosa pine (Pinus ponderosa) forest." International Journal of Wildland Fire 13, no. 2 (2004): 183. http://dx.doi.org/10.1071/wf03012.

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Forty-nine vegetation transects were measured in 1997 and 1998 to determine the impact of grass seeding after the 1996 Dome Fire, which burned almost 6900 ha of ponderosa pine (Pinus ponderosa Lawson) forest in the Jemez Mountains of north-central New Mexico. High- and moderate-burned areas in Santa Fe National Forest were seeded with a mixture that included the exotic ryegrass (Lolium multiflorum Lam.). Adjacent burned areas of Bandelier National Monument were not seeded, and were used as a control in the post-seeding study. On the seeded plots, foliar cover of ryegrass declined from 1997 to 1998 due to self-inhibition and/or reduced precipitation from 1997 to 1998. Foliar cover and diversity of native forbs were greater in 1997 than 1998, probably due to a wet growing season in 1997. Cover, species richness, and diversity of native forbs were highest in non-seeded areas of moderate- and high-burn intensities. Regeneration and survivorship of conifer seedlings decreased as ryegrass cover increased, particularly in areas of high-burn intensity. Exotic plant cover, mostly horseweed [Conyza canadensis (L.) Cronq.], increased from 1997 to 1998 in non-seeded areas of moderate- and high-burn intensity. Both the initial success of seeding and the eventual impacts on native vegetation were strongly modulated by climate variability.
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Smith, Monica L. "The archaeology of a “Destroyed” Site: Surface survey and historical documents at the civilian conservation corps camp, bandelier national monument, New Mexico." Historical Archaeology 35, no. 2 (June 2001): 31–40. http://dx.doi.org/10.1007/bf03374382.

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Sidman, Gabriel, D. Phillip Guertin, David C. Goodrich, Carl L. Unkrich, and I. Shea Burns. "Risk assessment of post-wildfire hydrological response in semiarid basins: the effects of varying rainfall representations in the KINEROS2/AGWA model." International Journal of Wildland Fire 25, no. 3 (2016): 268. http://dx.doi.org/10.1071/wf14071.

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Representation of precipitation is one of the most difficult aspects of modelling post-fire runoff and erosion and also one of the most sensitive input parameters to rainfall-runoff models. The impact of post-fire convective rainstorms, especially in semiarid watersheds, depends on the overlap between locations of high-intensity rainfall and areas of high-severity burns. One of the most useful applications of models in post-fire situations is risk assessment to quantify peak flow and identify areas at high risk of flooding and erosion. This study used the KINEROS2/AGWA model to compare several spatial and temporal rainfall representations of post-fire rainfall-runoff events to determine the effect of differing representations on modelled peak flow and determine at-risk locations within a watershed. Post-fire rainfall-runoff events at Zion National Park in Utah and Bandelier National Monument in New Mexico were modelled. Representations considered included both uniform and Soil Conservation Service Type II hyetographs, applying rain over the entire watershed and applying rain only on the burned area, and varying rainfall both temporally and spatially according to radar data. Results showed that rainfall representation greatly affected modelled peak flow, but did not significantly alter the model’s predictions for high-risk locations. This has important implications for post-fire assessments before a flood-inducing rainfall event, or for post-storm assessments in areas with low-gauge density or lack of radar data due to mountain beam blockage.
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Stone, Tammy. "An Analysis of Variability and Condition of Cavate Structures in Bandelier National Monument. H. Wolcott Toll. Intermountain Cultural Resources Center Professional Paper No. 53. U.S. Department of the Interior, National Park Service, Santa Fe, 1995. xvi + 300 pp., figures, tables, pull-out maps, appendixes, references, index. Paper (available on request)." American Antiquity 62, no. 1 (January 1997): 172. http://dx.doi.org/10.2307/282410.

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Dissertations / Theses on the topic "Bandelier National Monument"

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Stoffle, Richard W. "Bandelier National Monument A Study of Natural Resource Use among Culturally Affiliated Pueblo Communities." Bureau of Applied Research in Anthropology, University of Arizona, 2007. http://hdl.handle.net/10150/292608.

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This presentation is a summary key findings and recommendations for the Bandelier National Monument Traditional Use Study. This presentation was given by Dr. Stoffle during seperate meetings with National Park Service staff and the involved tribes.
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Books on the topic "Bandelier National Monument"

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H, Huey George H., and Southwest Parks and Monuments Association., eds. Bandelier National Monument. Tucson, Ariz: Southwest Parks and Monuments Association, 1990.

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Gustafson, Sarah. Exploring Bandelier National Monument. Tucson, Arizona: Southwest Parks and Monuments Association, 1996.

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Gustafson, Sarah. Exploring Bandelier National Monument. [Tucson, Ariz.]: Southwest Parks and Monuments Association, 1997.

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M, Ferguson William, and Ferguson Lisa, eds. Rock art of Bandelier National Monument. Albuquerque: University of New Mexico Press, 1989.

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Hoard, Dorothy. A guide to Bandelier National Monument. 4th ed. Los Alamos, NM: Los Alamos Historical Society, 2009.

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A guide to Bandelier National Monument. 3rd ed. Los Alamos, N.M: Los Alamos Historical Society, 1989.

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Rothman, Hal. Bandelier National Monument: An administrative history. Santa Fe, N.M: Southwest Cultural Resources Center, 1988.

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Smith, Monica L. The historic period at Bandelier National Monument. [Santa Fe, N.M.]: Anthropology Projects, Intermountain Support Office, Intermountain Region, National Park Service, Dept. of the Interior, 2002.

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Bandelier National Monument Cerro Grande prescribed fire investigation report. [Washington, D.C: U.S. Dept. of the Interior, National Park Service, 2000.

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Soullière, Laura E. Historic structure report, 1988: CCC buildings, Bandelier National Monument, New Mexico. [Denver]: U.S. Dept. of the Interior, National Park Service, Denver Service Center, 1991.

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Book chapters on the topic "Bandelier National Monument"

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"Bandelier National Monument." In The Americas, 58–61. Routledge, 2013. http://dx.doi.org/10.4324/9781315073828-17.

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Conference papers on the topic "Bandelier National Monument"

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Sica, Chelsea. "GROUND PENETRATING RADAR INVESTIGATION OF TYUONYI PUEBLO IN BANDELIER NATIONAL MONUMENT, NEW MEXICO." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303483.

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Veenhuis, Jack E. "The Effects of Wildfire on the Peak Streamflow Magnitude and Frequency, Frijoles and Capulin Canyons, Bandelier National Monument, New Mexico." In Watershed Management and Operations Management Conferences 2000. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40499(2000)39.

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Reports on the topic "Bandelier National Monument"

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Bogan, M. A., T. J. O`Shea, P. M. Cryan, A. M. Ditto, W. H. Schaedla, E. W. Valdez, K. T. Castle, and L. Ellison. A study of bat populations at Los Alamos National Laboratory and Bandelier National Monument, Jemez Mountains, New Mexico: FY95--97 report to Los Alamos National Laboratory and Bandelier National Monument. Office of Scientific and Technical Information (OSTI), December 1998. http://dx.doi.org/10.2172/296873.

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Jarmie, N., and F. J. Rogers. A survey of macromycete diversity at Los Alamos National Laboratory, Bandelier National Monument, and Los Alamos County; A preliminary report. Office of Scientific and Technical Information (OSTI), November 1997. http://dx.doi.org/10.2172/563252.

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Banar, Alethea K. Los Alamos National Laboratory 2018 Monitoring Season for storm water and atmospheric deposition samples from Bandelier National Monument under Permit # BAND-2018-SCI-0006 - 2018 Monitoring Season Summary. Office of Scientific and Technical Information (OSTI), February 2019. http://dx.doi.org/10.2172/1495121.

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Effects of Wildfire on the Hydrology of Capulin and Rito de los Frijoles canyons, Bandelier National Monument, New Mexico. US Geological Survey, 2002. http://dx.doi.org/10.3133/wri20024152.

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