How do Lava Plateaus Form?
The lava plains are made up of very wet basaltic mud during many successive eruptions using many holes without strong explosions (peaceful eruptions). This explosion is quiet due to the low viscosity of the lava and therefore very wet and contains a small number of trapped gases. The impact of lava flowsheet can be extracted from crevices or crevices in the lines or large volcanic cracks through many pre-historic pipelines that have produced large flood basalts. A series of massive mudslides covers the first area to form a plateau, which may contain volcanic mud fields, cinder clusters, protective volcanoes, and other types of volcanoes. In some cases, a volcano may be part of a single volcano. An example is the large Level Mountain shield in northern British Columbia, Canada, covering an area of 1,800 km2 (690 sq mi) and a volume of 860 km3 (210 cu mi). Probably the widest area of all the basaltic vessels that existed during the Paleogene period and probably extended over 1,800