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At the constructive plate margin, as I think you mean, largely basalt from extruded upper-Mantle material.

Examples are Iceland, the Giant's Causeway and the Isle of Staffa (host to Fingal's Cave). The latter two are flood-basalts from the early rifting that led to the Atlantic Ocean. Iceland is on the junction of two oceanic-ridge constructive margins: the Mid-Atlantic and the Reykjanes, Ridges.

Please someone correct me if the latter name is wrong - I did that from memory!

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12y ago

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