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- {{#forminput:form=Entry}}5 KB (501 words) - 20:50, 22 February 2017
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- {{#default_form:Entry}}{{NONUM}}32 bytes (4 words) - 15:43, 11 January 2017
- **initial entry172 bytes (17 words) - 12:34, 7 August 2015
File:C605-Figure-13.jpg ...approximately 2 ft (60 cm) long. (b) Close-up view on the west wall of the entry. The heart of the Galatia channel is south (left) of view. Notice how erosi(1,395 × 2,297 (822 KB)) - 15:53, 17 August 2023- === [[BibTeX]] entry ===3 KB (310 words) - 19:26, 5 December 2016
- ...ction needs to be taken. An informal unit requires the use of a different entry form. #:'''Wiki code tip:''' insert <nowiki><br></nowiki> at the end of each entry so a hard return is added to the wiki code2 KB (330 words) - 20:13, 3 February 2017
- For a complete rewrite of an entry, you can use our [[Form:Entry]]. Otherwise, minor edits can be added to the current page for any unit.<b2 KB (402 words) - 21:39, 30 November 2016
- #::"Entry" - for a normal approved unit3 KB (457 words) - 22:03, 7 February 2017
- {{#forminput:form=Entry}}5 KB (501 words) - 20:50, 22 February 2017
- ...e Formation level, as Kimmswick Limestone. A more complete update to this entry is in progress.'''<br>3 KB (472 words) - 19:56, 23 February 2024
- ...ous fluvial deposits and the rarity of gray shale clastic wedges (see next entry) place the setting low on the coastal plain.13 KB (1,879 words) - 16:37, 9 February 2022
- ...iment transport within channel systems is, of course, tied directly to the entry of sediment into drainage systems. As discussed by Cecil and Dulong (2003)<49 KB (7,357 words) - 14:48, 23 August 2023