{"id":431,"date":"2021-02-01T16:08:12","date_gmt":"2021-02-01T21:08:12","guid":{"rendered":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/?post_type=chapter&#038;p=431"},"modified":"2021-02-02T15:09:26","modified_gmt":"2021-02-02T20:09:26","slug":"exercise-4-2-intermediate-correlation-exercise","status":"publish","type":"chapter","link":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/chapter\/exercise-4-2-intermediate-correlation-exercise\/","title":{"raw":"Exercise 4.2. Intermediate Correlation Exercise","rendered":"Exercise 4.2. Intermediate Correlation Exercise"},"content":{"raw":"<h1>What To Do<\/h1>\r\n<p class=\"hanging-indent\">1. Refer to the printer-friendly worksheets you downloaded (<a href=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/part\/lab-4-stratigraphic-correlation\/\">available at the beginning of Lab 4<\/a>). You can also <a href=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10.png\" target=\"_blank\" rel=\"noopener noreferrer\">click here<\/a> to download Figure 4.10 as a PNG file for editing with drawing software.<\/p>\r\n<p class=\"hanging-indent\">2. Draw lithologic correlation lines to connect equivalent rock units (shown using Roman numerals) in Figure 4.10.<\/p>\r\n<p class=\"hanging-indent\">3. Using a different colour, draw lines connecting equivalent time-stratigraphic units. <span style=\"color: #800000\"><strong>The numbers beside the rock units correspond to time intervals.\u00a0<\/strong><\/span><\/p>\r\n<p class=\"hanging-indent\">4. Answer the questions that follow Figure 4.10.<\/p>\r\n\r\n\r\n[caption id=\"attachment_434\" align=\"alignnone\" width=\"1140\"]<a href=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/chapter\/exercise-4-2-intermediate-correlation-exercise\/f4-10\/\" rel=\"attachment wp-att-434\"><img class=\"size-full wp-image-434\" src=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10.png\" alt=\"\" width=\"1140\" height=\"795\" \/><\/a> <strong>Figure 4.10 |<\/strong> Stratigraphic columns for Exercise 4.2.[\/caption]\r\n<h3>Questions<\/h3>\r\n<p class=\"hanging-indent\">a. Identify the depositional environment of the following facies descriptions. Transcribe these environments onto Figure 4.10.<\/p>\r\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">i. The bedrock is granite gneiss.<\/p>\r\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">ii. Mature white quartz sandstone with crossbeds and Skolithos trace fossils.<\/p>\r\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">iii. Tan coloured shale and siltstone, some hummocky beds and Cruziana traces.<\/p>\r\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">iv.\u00a0 Light grey biomicrite with thinly laminated and hummocky beds.<\/p>\r\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">v. \u00a0 Black, thinly laminated shale with Zoophycus traces.<\/p>\r\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">vi.\u00a0 Dark grey shale and sandstone showing graded beds, and sole marks in cyclic bedding.<\/p>\r\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">vii. Greenish siltstones at base becoming tan medium sans with metre-scale crossbeds, rare shells.<\/p>\r\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">viii. Reddish brown, clast supported conglomerate interbedded with Crossbedded brown, immature coarse sandstone and mud-cracked siltstone.<\/p>\r\n<p class=\"hanging-indent\">b. What is happening to relative sea level between time intervals 1 and 4?<\/p>\r\n<p class=\"hanging-indent\">c. In which direction was the source for the sediment that forms unit (ii)?<\/p>\r\n<p class=\"hanging-indent\">d. Where would the deepest part of the sedimentary basin have been at time 1? Where would the shoreline have been?<\/p>\r\n<p class=\"hanging-indent\">e. Where is the deepest part of the basin (the lowest elevation) at time 4?<\/p>\r\n<p class=\"hanging-indent\">f. What was happening to relative sea level between time intervals 4 and 8?<\/p>\r\n<p class=\"hanging-indent\">g. Where was the shoreline at time 7? How did you come to this conclusion?<\/p>\r\n<p class=\"hanging-indent\">h. What does the appearance of (viii) directly on top of (vii) tell you about the sedimentary history of this region?<\/p>\r\n<p class=\"hanging-indent\">i. Could this whole sedimentary sequence be created by global sea level rise and fall only? What other processes could have occurred?<\/p>","rendered":"<h1>What To Do<\/h1>\n<p class=\"hanging-indent\">1. Refer to the printer-friendly worksheets you downloaded (<a href=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/part\/lab-4-stratigraphic-correlation\/\">available at the beginning of Lab 4<\/a>). You can also <a href=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10.png\" target=\"_blank\" rel=\"noopener noreferrer\">click here<\/a> to download Figure 4.10 as a PNG file for editing with drawing software.<\/p>\n<p class=\"hanging-indent\">2. Draw lithologic correlation lines to connect equivalent rock units (shown using Roman numerals) in Figure 4.10.<\/p>\n<p class=\"hanging-indent\">3. Using a different colour, draw lines connecting equivalent time-stratigraphic units. <span style=\"color: #800000\"><strong>The numbers beside the rock units correspond to time intervals.\u00a0<\/strong><\/span><\/p>\n<p class=\"hanging-indent\">4. Answer the questions that follow Figure 4.10.<\/p>\n<figure id=\"attachment_434\" aria-describedby=\"caption-attachment-434\" style=\"width: 1140px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/chapter\/exercise-4-2-intermediate-correlation-exercise\/f4-10\/\" rel=\"attachment wp-att-434\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-434\" src=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10.png\" alt=\"\" width=\"1140\" height=\"795\" srcset=\"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10.png 1140w, https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10-300x209.png 300w, https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10-1024x714.png 1024w, https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10-768x536.png 768w, https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10-65x45.png 65w, https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10-225x157.png 225w, https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-content\/uploads\/sites\/1224\/2021\/02\/F4-10-350x244.png 350w\" sizes=\"auto, (max-width: 1140px) 100vw, 1140px\" \/><\/a><figcaption id=\"caption-attachment-434\" class=\"wp-caption-text\"><strong>Figure 4.10 |<\/strong> Stratigraphic columns for Exercise 4.2.<\/figcaption><\/figure>\n<h3>Questions<\/h3>\n<p class=\"hanging-indent\">a. Identify the depositional environment of the following facies descriptions. Transcribe these environments onto Figure 4.10.<\/p>\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">i. The bedrock is granite gneiss.<\/p>\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">ii. Mature white quartz sandstone with crossbeds and Skolithos trace fossils.<\/p>\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">iii. Tan coloured shale and siltstone, some hummocky beds and Cruziana traces.<\/p>\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">iv.\u00a0 Light grey biomicrite with thinly laminated and hummocky beds.<\/p>\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">v. \u00a0 Black, thinly laminated shale with Zoophycus traces.<\/p>\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">vi.\u00a0 Dark grey shale and sandstone showing graded beds, and sole marks in cyclic bedding.<\/p>\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">vii. Greenish siltstones at base becoming tan medium sans with metre-scale crossbeds, rare shells.<\/p>\n<p class=\"hanging-indent\" style=\"padding-left: 40px\">viii. Reddish brown, clast supported conglomerate interbedded with Crossbedded brown, immature coarse sandstone and mud-cracked siltstone.<\/p>\n<p class=\"hanging-indent\">b. What is happening to relative sea level between time intervals 1 and 4?<\/p>\n<p class=\"hanging-indent\">c. In which direction was the source for the sediment that forms unit (ii)?<\/p>\n<p class=\"hanging-indent\">d. Where would the deepest part of the sedimentary basin have been at time 1? Where would the shoreline have been?<\/p>\n<p class=\"hanging-indent\">e. Where is the deepest part of the basin (the lowest elevation) at time 4?<\/p>\n<p class=\"hanging-indent\">f. What was happening to relative sea level between time intervals 4 and 8?<\/p>\n<p class=\"hanging-indent\">g. Where was the shoreline at time 7? How did you come to this conclusion?<\/p>\n<p class=\"hanging-indent\">h. What does the appearance of (viii) directly on top of (vii) tell you about the sedimentary history of this region?<\/p>\n<p class=\"hanging-indent\">i. Could this whole sedimentary sequence be created by global sea level rise and fall only? What other processes could have occurred?<\/p>\n","protected":false},"author":1019,"menu_order":5,"template":"","meta":{"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[48],"contributor":[],"license":[],"class_list":["post-431","chapter","type-chapter","status-publish","hentry","chapter-type-numberless"],"part":163,"_links":{"self":[{"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/pressbooks\/v2\/chapters\/431","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/wp\/v2\/users\/1019"}],"version-history":[{"count":8,"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/pressbooks\/v2\/chapters\/431\/revisions"}],"predecessor-version":[{"id":479,"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/pressbooks\/v2\/chapters\/431\/revisions\/479"}],"part":[{"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/pressbooks\/v2\/parts\/163"}],"metadata":[{"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/pressbooks\/v2\/chapters\/431\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/wp\/v2\/media?parent=431"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/pressbooks\/v2\/chapter-type?post=431"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/wp\/v2\/contributor?post=431"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/earthhistorylab\/wp-json\/wp\/v2\/license?post=431"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}