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首页> 外文期刊>The Mountain Geologist >A Survey of Fossils and Geology of Red Rock Canyon Open pace,Colorado Springs, Colorado
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A Survey of Fossils and Geology of Red Rock Canyon Open pace,Colorado Springs, Colorado

机译:科罗拉多科罗拉多斯普林斯红色岩石峡谷开放步伐的化石和地质调查

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摘要

Red Rock Canyon Open Space (RRCOS) is a 785-acre open space in the western foothills of ColoradoSprings, Colorado. The City of Colorado Springs opened RRCOS to the public in October 2003. Becausethis acreage has been in private ownership since the late 1800s, there has been little documentation offossils or geology within this property. Although continuous with the stratigraphy of nearby Garden of the Gods Park, the geology ofRRCOS shows remarkable differences. Of primary significance are the relatively uninterrupted, upturnedexposures of a sequence of strata comprised of the Fountain Formation, Lyons Sandstone, Morrison andRalston Creek formations, Purgatoire Formation, Dakota Sandstone, the Benton Shale, Niobrara Forma-tion and Pierre Shale. The majority of formations can be seen within a 1.5 kilometer (km) west to easttransect. Lying horizontally over these vertical beds are the Mesa Gravels (equivalent to Verdos Allu-vium). Within these formations several sites of geologic interest to the Colorado Springs community wererecorded, in particular, the spectacular eolian crossbeds within the Lyons Sandstone. Fossils documented through this study include apparent roots within the Fountain Formation, andnumerous tree imprints, leaves, and Ankylosaurid and Iguanodontid tracks in the Dakota Sandstone. TheCodell Sandstone and Niobrara Formation display shark and fish teeth, ammonites, inoceramids, a possi-ble Mosasaur palatine tooth, and tail or fin rays of an Ichthyodectes sp. fish.
机译:红岩峡谷休憩用地(RRCOS)是一个占地785英亩的休憩用地,位于科罗拉多州科罗拉多斯普林斯的西山麓。科罗拉多斯普林斯市于2003年10月向公众开放RRCOS。由于该土地自1800年代后期以来一直为私人所有,因此该物业内几乎没有文件化石或地质资料。尽管与附近的众神公园花园地层连续,但RRCOS的地质表现出显着差异。最主要的意义是一系列地层的相对不间断,上倾的暴露,包括喷泉组,里昂砂岩,莫里森和罗尔斯顿克里克组,普尔加图尔组,达科他砂岩,本顿页岩,尼奥布拉拉地层和皮埃尔页岩。可以看到大多数地层在西至东断面1.5公里(km)内。 Mesa Gravels(相当于Verdos Allu-vium)水平躺在这些垂直床上。在这些地层中,记录了科罗拉多斯普林斯社区的几处地质景点,特别是里昂砂岩中壮观的风积交错层。通过这项研究记录的化石包括泉源地层中的明显根部,以及达科他砂岩中无数的树印,树叶以及甲龙和蜥脚类动物的踪迹。 Codell砂岩和Niobrara岩层显示出鲨鱼和鱼齿,炸药,蛇骨石,可能的Mosasaur ala齿以及鱼鳞ect的尾鳍或鳍鳍。鱼。

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