Lorne plateau lavas
In today's world, Lorne plateau lavas has gained great relevance, generating a significant impact on various aspects of daily life. Since its emergence, Lorne plateau lavas has sparked endless debates and conflicting opinions, becoming a topic of general interest that has captured the attention of millions of people around the world. It doesn't matter if Lorne plateau lavas is in the field of politics, science, culture, or any other field, its influence is undeniable and its presence is constant on a daily basis. In this article, we will explore the various facets of Lorne plateau lavas and its impact on our society today.
The Lorne plateau lavas are basaltic lava flows extruded in the late Silurian, 424 to 415 million years ago, which are found today in the Oban - Kerrera area of Scotland. Peperite occurs where they flowed into Old Red Sandstone lakes.
References
- ^ Stampfli, G.M. (2002). "A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons". Earth and Planetary Science Letters. 196 (1): 17–33. Bibcode:2002E&PSL.196...17S. doi:10.1016/S0012-821X(01)00588-X.
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