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<br />e <br /> <br />e <br /> <br />e <br /> <br />3-21 <br /> <br />to be developed in tentative form during the preliminary investigation <br />of the site. With the benefit of the additional information obtained <br />during logging and sampling, the original profile is to be refined to <br />include more precise information on the extent, thickness and position <br />in the profile of stratigraphic units. The survey stationing, bank <br />line, and proposed invert level are to be plotted, as are the locations <br />and logs of pits or drill holes. The upper and lower elevations of <br />stratigraphic units will be shown at the appropriate station site. <br />When the correlation of units between pit or drill hole sites has been <br />determined, correlation lines are drawn as shown on Figure 3-4. In <br />this example, it is implied that correlation between test hole sites <br />has been. facilitated by exposures in stream banks. Additional test <br />holes would be required where such exposures are not available. <br /> <br />The "U" on the right of the profile test hole location indicates that <br />an undisturbed sample was obtained. A disturbed sample mayor may not <br />be obtained at the same site depending upon whether enough material is <br />available in the undisturbed sample-for classification. The investi- <br />gators have identified this stratigraphic unit as consisting of soil <br />which would resist erosion as a mass rather than as discrete particles. <br />The "D" indicates that a disturbed sample has been obtained. The <br />investigators have made a field determination that the unit is non- <br />coherent and that erosion characteristics are dependent on the indi- <br />vidual particle characteristics. The stratigraphic unit delineations <br />on Figure 3-4 are not dependent on the indicated investigation sites <br />alone but include determinations from observations along stream banks <br />and from hand borings. When the test data have been obtained, results <br />pertinent to the erosion or stability characteristics may be shown or <br />listed on attached report sheets with the data clearly identified with <br />the appropriate units. Ground water, if encountered, should be shown <br />at each of the investigation test hole locations. <br /> <br />The longitudinal profile with stratigraphic unit interpretations is <br />primarily for purposes of stability evaluation, and without it the <br />designer does not know that interpretations of soil characteristics <br />have been made between investigation sites. <br /> <br />The logs of test pits or drill holes and the plan map showing the <br />location of these investigation sites should accompany the profiles as <br />supporting and supplemental information and a copy will be placed in <br />the design folio. <br /> <br />The geologic profile and plan map should show the locations and the <br />extent of outcropping bedrock. They should also show its verified or <br />estimated depth below the present streambed and its relation to the <br />proposed channel invert. Existing erosion or deposition features <br />associated with the outcrop (either up or down stream) should also be <br />shown. <br />