{"id":903,"date":"2021-09-16T19:31:02","date_gmt":"2021-09-16T19:31:02","guid":{"rendered":"https:\/\/pressbooks.ccconline.org\/physicalgeology\/chapter\/versioning-history-physical-geology-2nd-edition\/"},"modified":"2021-09-16T19:43:24","modified_gmt":"2021-09-16T19:43:24","slug":"versioning-history-physical-geology-2nd-edition","status":"publish","type":"chapter","link":"https:\/\/pressbooks.ccconline.org\/physicalgeology\/chapter\/versioning-history-physical-geology-2nd-edition\/","title":{"raw":"Versioning History -- Physical Geology – 2nd Edition","rendered":"Versioning History — Physical Geology – 2nd Edition"},"content":{"raw":"\n\n

7<\/h3>

Versioning History<\/h1><\/div>
\n <!-- pb_fixme -->\n

This page provides a record of edits and changes made to this book since its initial publication in the B.C. Open Textbook Collection<\/a>. Whenever edits or updates are made, we make the required changes in the text and provide a record and description of those changes here. If the change is minor, the version number increases by 0.01. However, if the edits involve substantial updates, the version number goes up to the next full number. The files on our website always reflect the most recent version, including the print-on-demand copy.<\/p>\n

If you find an error in this book, please fill out the Report an Open Textbook Error<\/a><\/span> form.<\/p>\n
Version<\/th> Date<\/th> Change<\/th> Details<\/th> <\/tr>
2.00<\/td> September 23, 2019<\/td> Added to the B.C. Open Textbook Collection.<\/td> <\/td><\/tr>
2.01<\/td> January 27, 2020<\/td> Error correction.<\/td> Applied superscripts to numbers in Table 22.3 in Chapter 22.3.

Fixed broken links in Glossary.<\/p><\/td> <\/tr>

2.02<\/td> May 7, 2020<\/td> Error correction.<\/td> Updated Darcy\u2019s equation for estimating the volume of groundwater flow in Chapter 14.2. Altered Exercise 14.1 and its answer in Appendix 3.<\/td> <\/tr>
2.03<\/td> June 10, 2020<\/td> Error correction.<\/td> Replaced Figure 9.1.4 and edited a following bullet point from \u201cS waves do not pass through the outer part of the core.\u201d to \u201cS waves do not pass through the outer liquid part of the core, but S waves can be created by P waves at the surface of the inner core and their inner core velocity is 3.6 km\/s.\u201d<\/td> <\/tr>
2.04<\/td> September 22, 2020<\/td> Error correction.<\/td> In Exercise 2.1 in Chapter 2.2, the atomic number of beryllium was changed from 3 to 4.<\/td> <\/tr>
2.05<\/td> January 21, 2021<\/td> Error corrections.<\/td> In Exercise 7.4, replaced the image and fixed broken link. Added answers to the Rock and Mineral Review Exercise to Appendix 3. Made corrections to Chapter 14\u2019s Questions for Review question #5 and updated answer numbering.<\/td> <\/tr>
2.06<\/td> February 26, 2021<\/td> Error correction.<\/td> In Section 16.4 the sentence \u201cSupraglacial (on top of the ice) and Supraglacial<\/strong> (within the ice) sediments that slide off the melting front of a stationary glacier can form a ridge of unsorted sediments called an englacial<\/strong>.\u201d was corrected to \u201cSupraglacial (on top of the ice) and englacial<\/strong> (within the ice) sediments that slide off the melting front of a stationary glacier can form a ridge of unsorted sediments called a terminal moraine<\/strong>.\u201d<\/td> <\/tr> <\/tbody> <\/table>\n <!-- pb_fixme -->\n<\/div>\n<\/div>
\n <!-- pb_fixme -->\n <!-- pb_fixme -->\n<\/div>\n<\/div>\n","rendered":"
\n
\n

7<\/h3>\n

Versioning History<\/h1>\n<\/div>\n
\n
\n <!– pb_fixme –><\/p>\n

This page provides a record of edits and changes made to this book since its initial publication in the B.C. Open Textbook Collection<\/a>. Whenever edits or updates are made, we make the required changes in the text and provide a record and description of those changes here. If the change is minor, the version number increases by 0.01. However, if the edits involve substantial updates, the version number goes up to the next full number. The files on our website always reflect the most recent version, including the print-on-demand copy.<\/p>\n

If you find an error in this book, please fill out the Report an Open Textbook Error<\/a><\/span> form.<\/p>\n\n\n\n\n\n\n\n\n\n\n
Version<\/th>\nDate<\/th>\nChange<\/th>\nDetails<\/th>\n<\/tr>\n
2.00<\/td>\nSeptember 23, 2019<\/td>\nAdded to the B.C. Open Textbook Collection.<\/td>\n <\/td>\n<\/tr>\n
2.01<\/td>\nJanuary 27, 2020<\/td>\nError correction.<\/td>\nApplied superscripts to numbers in Table 22.3 in Chapter 22.3. <\/p>\n

Fixed broken links in Glossary.<\/p>\n<\/td>\n<\/tr>\n

2.02<\/td>\nMay 7, 2020<\/td>\nError correction.<\/td>\nUpdated Darcy\u2019s equation for estimating the volume of groundwater flow in Chapter 14.2. Altered Exercise 14.1 and its answer in Appendix 3.<\/td>\n<\/tr>\n
2.03<\/td>\nJune 10, 2020<\/td>\nError correction.<\/td>\nReplaced Figure 9.1.4 and edited a following bullet point from \u201cS waves do not pass through the outer part of the core.\u201d to \u201cS waves do not pass through the outer liquid part of the core, but S waves can be created by P waves at the surface of the inner core and their inner core velocity is 3.6 km\/s.\u201d<\/td>\n<\/tr>\n
2.04<\/td>\nSeptember 22, 2020<\/td>\nError correction.<\/td>\nIn Exercise 2.1 in Chapter 2.2, the atomic number of beryllium was changed from 3 to 4.<\/td>\n<\/tr>\n
2.05<\/td>\nJanuary 21, 2021<\/td>\nError corrections.<\/td>\nIn Exercise 7.4, replaced the image and fixed broken link. Added answers to the Rock and Mineral Review Exercise to Appendix 3. Made corrections to Chapter 14\u2019s Questions for Review question #5 and updated answer numbering.<\/td>\n<\/tr>\n
2.06<\/td>\nFebruary 26, 2021<\/td>\nError correction.<\/td>\nIn Section 16.4 the sentence \u201cSupraglacial (on top of the ice) and Supraglacial<\/strong> (within the ice) sediments that slide off the melting front of a stationary glacier can form a ridge of unsorted sediments called an englacial<\/strong>.\u201d was corrected to \u201cSupraglacial (on top of the ice) and englacial<\/strong> (within the ice) sediments that slide off the melting front of a stationary glacier can form a ridge of unsorted sediments called a terminal moraine<\/strong>.\u201d<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

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