1990
DOI: 10.1080/03122417.1990.11681367
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Blowing in The Wind. Slte Destruction and Slte Creation at Hawker Lagoon, South Australia

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Cited by 15 publications
(6 citation statements)
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“…The data from CA-SMI-87 corroborate the findings of previous studies by Brown (1985), Cameron et al (1990), Leach et al (1998), Wandsnider (1988, and others, demonstrating that eolian disturbances are integrally linked to vegetation and ground cover, with those areas that are generally well covered exhibiting the best preservation. The data from CA-SMI-87, however, indicate that archaeologists cannot assume that because site deposits, including stratified shell middens exhibiting vertical variation, are presently covered with vegetation or sediment that those deposits have always been sealed.…”
Section: Discussionsupporting
confidence: 93%
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“…The data from CA-SMI-87 corroborate the findings of previous studies by Brown (1985), Cameron et al (1990), Leach et al (1998), Wandsnider (1988, and others, demonstrating that eolian disturbances are integrally linked to vegetation and ground cover, with those areas that are generally well covered exhibiting the best preservation. The data from CA-SMI-87, however, indicate that archaeologists cannot assume that because site deposits, including stratified shell middens exhibiting vertical variation, are presently covered with vegetation or sediment that those deposits have always been sealed.…”
Section: Discussionsupporting
confidence: 93%
“…Working in west Texas and southern New Mexico, Leach et al (1998) also documented the role of wind in structuring the size, content, and formation of lithic scatters in the area. In Australia, Cameron et al (1990) noted the eolian destruction of in situ deposits, as well as the creation of new secondary sites by eolian deposition. Based on experiments conducted in South African dune fields, lithics, particularly small ones, moved relatively rapidly because of deflation (Lancaster, 1986).…”
Section: Discussionmentioning
confidence: 98%
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“…Entre los atributos de estas concentraciones, se observa una reducida variabilidad de tamaños y una densidad superior a la observada en sus alrededores (7 artefactos/m 2 vs 0,55 artefactos/m 2 , respectivamente). Entonces, en las planicies eololacustres la presencia de artefactos de tamaños pequeños no puede ser considerada un proxy de la integridad del conjunto como sí puede serlo en espacios afectados fundamentalmente por la acción eólica (aunque ver Cameron et al 1990). Aquí el efecto más importante del viento es la generación del oleaje y el "arrinconamiento" del agua de la laguna sobre las márgenes orientales.…”
Section: Resultsunclassified
“…These aeolian sand dunes contain the archaeological material product of human occupations that took place in a dune setting or ancient marine terraces which are covered by aeolian sediments (Mayer 2002). Due to wind erosion, and the deflation processes it causes, the archaeological record was alternatively buried and exposed (Cameron et al 1990;Fanning & Holdaway 2001;Favier Dubois et al 2008). Previous work in the area indicated the presence of a blowout dune, a collapsed dune profile and surface scatters (Gómez Otero 2006).…”
Section: Introductionmentioning
confidence: 99%