Download Stratigraphy and paleoenvironments of Late Quaternary valley by Vance T. Holliday PDF
By Vance T. Holliday
Read Online or Download Stratigraphy and paleoenvironments of Late Quaternary valley fills on the southern High Plains PDF
Similar geology books
Stanford Geological Atlas Of Great Britain And Ireland -1907
Excerpt from Stanford's Geological Atlas of serious Britain and eire: With Plates of attribute FossilsThe scope of this paintings has been enlarged via the addition of a comic strip of the geological gains of eire, its counties and major strains of railway; and the topic is illustrated through a geological map of the rustic, and by way of 3 illustrations borrowed from Professor E.
This quantity is a set of papers, preceded by means of an introductory essay, on coastal physiography. the entire authors have made major contributions to the topic. they're of other nationalities and the papers are, intentionally, now not all fresh ones. during this ebook emphasis has been laid totally on issues that are of basic instead of neighborhood or maybe nearby price.
- Introducing Geology: A Guide to the World of Rocks
- Groundwater Age
- AGI Data Sheets: For Geology in the Field Laboratory and Office
- Surf, Sand, and Stone: How Waves, Earthquakes, and Other Forces Shape the Southern California Coast
- Slope Tectonics (Geological Society Special Publication 351)
Extra info for Stratigraphy and paleoenvironments of Late Quaternary valley fills on the southern High Plains
Sample text
White et al. (1946, p. 387) noted that peak flood flow in May 1937 along Running Water Draw at Plainview was 1,200 cubic feet per second while the maximum flow 15 miles downstream was 80 cubic feet per second. Stafford (1981) proposed that spring-fed ponds and marshes may be associated with deeply entrenched, highly sinuous meanders of draws, based mostly on geoarchaeological studies in lower Yellowhouse Draw at and below Lubbock Lake. The present study provides no evidence of a relationship between the location of springs and entrenched meanders.
TABLE 11C. LITHOLOGIC AND PEDOLOGIC CHARACTERISTICS OF LOWER MUSTANG DRAW Stratum/ Soil Range in Thickness (cm) TABLE 12. LITHOLOGIC AND PEDOLOGIC CHARACTERISTICS OF MIDLAND DRAW Description Stratum/ Soil Range in Thickness (cm) Description Lubbock Lake soil A (ochric) - Bw or Bk (cambic and Stage I-II calcic); locally Bt/Btk argillic and calcic. 4 4s: L, SL; silty locally. Lubbock Lake soil A (ochric) - Bt-Btk (argillic and Stage I-II calcic). Yellowhouse soil 3c: A (ochric, locally cumulic) - C 4 4s: SCL, L, CL 3 25 - 240 3c: SiL, CL, L, SCL; 16-61% carb.
Ence with Blackwater (Fig. 20F). A likely equivalent of stratum 5m was found in lower Sulphur Springs Draw (stratum 6; Fredrick, 1994). In lower Yellowhouse and lower Sulphur Springs Draws, 5m locally is inset into older deposits (Fig. 28B). There are localized accumulations of silty, sandy, and sandy gravel facies (5s), and gravelly facies (5g) of stratum 5 along both the valley axes and valley margins. The most extensive accumulations are known from Plainview (Running Water Draw), Lubbock Landfill (Blackwater Draw), and Lubbock Lake (Yellowhouse Draw), where large exposures are accessible (Figs.