Talk:Socompa/GA1

GA Review
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Reviewer: Mike Christie (talk · contribs) 23:11, 3 March 2018 (UTC)

I'll review this. Mike Christie (talk - contribs - library) 23:11, 3 March 2018 (UTC)

I'll copyedit as I go through; please revert as needed.
 * its large debris avalanche deposit, which was formed 7,200 years ago when most of the northwestern slope collapsed and slid down, forming a large deposit: "large...deposit...large deposit".
 * Rewritten.


 * A large wedge-shaped scar is recognizable on the northwestern flank, with prominent scarps running through the western and northern flanks of the edifice forming its delimitation: suggest "A large wedge-shaped scar is recognizable on the northwestern flank, delimited by prominent scarps running through the western and northern flanks of the edifice".
 * Rewritten.


 * The summit of the volcano was cut by the collapse and some lava domes embedded within the volcano exposed in the rim of the collapse amphitheatre: if I'm reading this correctly, I'd suggest "were exposed" as easier to parse.
 * Fixed.

-- More to come. Mike Christie (talk - contribs - library) 23:49, 3 March 2018 (UTC)
 * Did some edits. Jo-Jo Eumerus (talk, contributions) 10:27, 4 March 2018 (UTC)

Continuing: -- Mike Christie (talk - contribs - library) 11:07, 4 March 2018 (UTC)
 * A spaceborne image of the region northwest of Socompa, which is recognizable in the lower left tip: if Socompa is lower left, isn't this the region northeast of Socompa? Or is north to the right here?
 * Is there a link for lineament?
 * Suggest moving the link for basement to first use.
 * contain biotite and andesites olivine: should this be "biotite, andesites, and olivine"?
 * Got them. Jo-Jo Eumerus (talk, contributions) 11:29, 4 March 2018 (UTC)
 * Promoting. Mike Christie (talk - contribs - library) 11:39, 4 March 2018 (UTC)