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An Archaeological Survey of a Pipeline Route Near Sabine Pass, Jefferson County, Texas

机译:德克萨斯州杰斐逊县萨宾山口附近管道线路的考古调查

摘要

In May 1980, the Center for Archaeological Research, The University of Texas at San Antonio, carried out an archaeological survey of the proposed route of an eight-inch pipeline to be installed by the Tennessee Gas Pipeline Company. The pipeline will extend from the Scurlock Oil Company tank farm about one kilometer southwest of Sabine Pass to a landfall on the Gulf Coast at a point about six kilometers west of Texas Point (Fig. 1).The survey was done under contract between the Center for Archaeological Research and the Tennessee Gas Pipeline Company (Independent Contractor-Letter Agreement of May 1980). The fieldwork was carried out by Kenneth M. Brown, Research Associate, under the supervision of Dr. Thomas R. Hester, Center Director, and Jack D. Eaton, Associate Director.The pipeline route is about 4.6 km long; crossing the chenier plain with a north-south orientation. The chenier plain consists of long, low sand and shell ridges, or cheniers, subparallel to the present coast, alternating with saline or brackish marsh and mudflats (Fisher et ale 1973; Kane 1959; Byrne, LeRoy, and Riley 1959). The area is also dotted with many elongate to irregular ponds. Ground visibility during the survey was fair to good on the cheniers, especially on the seaward side where the coarsest sediments were exposed; sandy deflated surfaces are common there. Washovers where the cheniers have been breached during high water also offered good visibility. The marsh between the cheniers, although dry enough during the survey to walk on in most places, is heavily vegetated, with a substrate of wet silt, clay, and organic muck. Ground visibility here was very unfavorable.
机译:1980年5月,得克萨斯大学圣安东尼奥分校考古研究中心对田纳西州天然气管道公司将安装的8英寸管道的拟建路线进行了考古调查。该管道将​​从Scurlock石油公司的油库延伸至Sabine Pass西南约一公里处,到达德克萨斯州以西约六公里处的墨西哥湾沿岸登陆区(图1)。考古研究和田纳西州天然气管道公司(1980年5月的独立承包商-信件协议)。现场工作由研究助理肯尼思·布朗(Kenneth M. Brown)在中心主任Thomas R. Hester博士和副主任Jack D. Eaton的监督下进行。管线全长约4.6公里;以南北方向穿过雪尼尔平原。谢尼尔平原由长而低的沙子和贝壳脊或谢尼尔组成,与当前海岸平行,与盐碱或咸淡的沼泽和滩涂交替出现(Fisher等,1973; Kane,1959; Byrne,LeRoy和Riley,1959)。该地区还散布着许多细长到不规则的池塘。在调查期间,地面能见度在雪尼尔上相当好,尤其是在暴露最粗的沉积物的海边。沙质的def缩表面在那儿很常见。在高水位时已弄坏了衬套的冲洗效果也很明显。尽管在调查中,雪尼尔之间的沼泽虽然足够干燥,可以在大多数地方行走,但植被茂密,底泥是湿的粉砂,粘土和有机泥土。这里的地面可见度非常不利。

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    Brown Kenneth M.;

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