Jump to content

Qinghai Lake: Revision history


For any version listed below, click on its date to view it. For more help, see Help:Page history and Help:Edit summary. (cur) = difference from current version, (prev) = difference from preceding version, m = minor edit, → = section edit, ← = automatic edit summary

(newest | oldest) View (newer 50 | ) (20 | 50 | 100 | 250 | 500)

30 April 2024

10 April 2024

26 May 2023

11 May 2023

10 May 2023

16 February 2023

4 January 2023

15 December 2022

10 November 2022

15 July 2022

20 June 2022

28 January 2022

31 December 2021

31 October 2021

19 September 2021

5 September 2021

10 May 2021

6 March 2021

2 February 2021

26 November 2020

25 November 2020

23 October 2020

22 October 2020

14 October 2020

10 October 2020

24 September 2020

20 September 2020

19 September 2020

3 September 2020

20 August 2020

17 August 2020

16 August 2020

13 August 2020

30 July 2020

  • curprev 06:0906:09, 30 July 2020189.217.57.93 talk 22,886 bytes +171 →‎Geography: A basic feature of every endorheic basin, is the lowest point on its rim, i.e. the lowest pass out of the basin, and therefore the place where overflow would occur should there be a climatic shift favoring precipitation over evaporation in the basin. My edit identifies that point and its elevation. While it is most probably the point where overflowed occurred 150,000 years ago, that would need to be confirmed by more detailed investigation. undo Tag: Visual edit

12 July 2020

28 May 2020

(newest | oldest) View (newer 50 | ) (20 | 50 | 100 | 250 | 500)