Large igneous provinces, such as
Iceland, the
Siberian Traps,
Deccan Traps, and the
Ontong Java Plateau, are extensive regions of
basalts on a continental scale resulting from
flood basalt eruptions. When created, these regions often occupy several thousand square kilometres and have volumes on the order of millions of cubic kilometers. In most cases, the lavas are normally laid down over several million years. They release large amounts of gases. The
Réunion hotspot produced the Deccan Traps about 66 million years ago, coincident with the
Cretaceous–Paleogene extinction event. The scientific consensus is that
an asteroid impact was the cause of the extinction event, but the volcanic activity may have caused environmental stresses on extant species up to the
Cretaceous–Paleogene boundary. Some scientists have hypothesised that the volcanism around the Deccan Traps could have been intensified by the Chicxulub impact, which would have been close to the
antipodal point of the Traps at that time. Additionally, the largest flood basalt event (the Siberian Traps) occurred around 250 million years ago and was coincident with the largest mass extinction in history, the
Permian–Triassic extinction event, although it is unknown whether it was solely responsible for the extinction event. Such outpourings are not explosive, though
lava fountains may occur. Many volcanologists consider
Iceland to be a large igneous province that is currently being formed. The last major outpouring occurred in 1783–84 from the
Laki fissure, which is approximately long. An estimated of basaltic lava was poured out during the eruption (VEI 4). The Ontong Java Plateau has an area of about , and the province was at least 50% larger before the
Manihiki and
Hikurangi Plateaus broke away. == Massive explosive eruptions ==