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Did the taste of ocean water (seawater) somewhat change due to ocean acidification when compared between pre-industrial and modern periods (say 18th and 21st centuries)? 212.180.235.46 ( talk) 14:35, 20 February 2020 (UTC)
Does someone know a source - or several - which relate the volume of a dyke or intrusion with that of the associated lava flow, such as would be expected during a volcanic eruption where some magma stays in the conduit? Note that I am not asking about the ratio of intrusive vs extrusive rocks in general, only these that are part of a discrete eruption event. Jo-Jo Eumerus ( talk) 18:47, 20 February 2020 (UTC)
Science desk | ||
---|---|---|
< February 19 | << Jan | February | Mar >> | February 21 > |
Welcome to the Wikipedia Science Reference Desk Archives |
---|
The page you are currently viewing is a transcluded archive page. While you can leave answers for any questions shown below, please ask new questions on one of the current reference desk pages. |
Did the taste of ocean water (seawater) somewhat change due to ocean acidification when compared between pre-industrial and modern periods (say 18th and 21st centuries)? 212.180.235.46 ( talk) 14:35, 20 February 2020 (UTC)
Does someone know a source - or several - which relate the volume of a dyke or intrusion with that of the associated lava flow, such as would be expected during a volcanic eruption where some magma stays in the conduit? Note that I am not asking about the ratio of intrusive vs extrusive rocks in general, only these that are part of a discrete eruption event. Jo-Jo Eumerus ( talk) 18:47, 20 February 2020 (UTC)