http://earthwise-staging.bgs.ac.uk/index.php?action=history&feed=atom&title=File%3AGSG_GLA_FIG_25_14.jpg 2026-04-19T06:24:16Z Revision history for this page on the wiki MediaWiki 1.42.3 http://earthwise-staging.bgs.ac.uk/index.php?title=File:GSG_GLA_FIG_25_14.jpg&diff=39621&oldid=prev 2019-02-11T17:14:27Z

<p>User created page with UploadWizard</p> <p><b>New page</b></p><div>=={{int:filedesc}}==<br /> {{Information<br /> |description={{en|1=Figure 25.14. Explanation of the sediment-lava cycles in the Pinbain Block and elsewhere. When the rate of lava extrusion is rapid or the rate of sea-level change is slow, the lavas advance into the sea. Because of seawater-lava interactions, where the lavas break down by explosive or erosional activity, lavas are always associated with tongues of lava entirely enclosed in breccia. However further towards the source of the lavas there are fewer breccia deposits. Shales and cherts on the other hand accumulate in deeper water and associated with them are tuffs which were deposited there either by air-fall (from explosive activity), storm deposition or turbidites. When volcanic activity has ceased or is waning the sea transgresses over the lavas to yield well rounded conglomerates, sometimes with reddened clasts if the lavas have been subject to subaerial exposure. This association of lava and breccia is common in nearly all the major lava sequences at Ballantrae, and in this Pinbain section massive lavas characterize Pinbain Hill; interfingers of breccias and lavas are seen on the coastal section (Localities 1–10). Transgressive conglomerates are seen at Localities 2 and 7).<br /> {{GSGGlasgow}}}}<br /> |date=2019-02-11 17:05:45<br /> |source=Geological Society of Glasgow<br /> |author=Geological Society of Glasgow<br /> |permission=<br /> |other versions=<br /> }}<br /> <br /> =={{int:license-header}}==<br /> {{subst:Custom license marker added by UW}}<br /> {{GSG1}}<br /> <br /> [[Category:Uploaded with UploadWizard]]</div>

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