in various parts of the area; it is in the center, where the thickness is the greatest, where it is possible that the magma is being fed to the Rajmahal Traps up above. Presence of underplating is also found in the Cambay rift at the depth range of 25 and 31 km through gravity modeling. Denudation In the British Isles, (Paleogene) denudation is linked with magmatic underplating. It has been shown that the wavelength and amplitude of denudation can be determined by the density and distribution of the underplating in a given area. Modeling of data brought on by studies of the British Isles shows that a large amount of high velocity material occurs around the Mohorovičić discontinuity under the Irish Sea. Epeirogenic uplift is a long-wavelength form of uplift and be split up into two separate categories, which is transient and permanent. Permanent epeirogenic uplift is possibly mainly produced by magmatic underplating, while transient uplift is more involved with mantle convection. Magmatic underplating is important for causing quick epeirogenic uplift in certain areas. It has been argued that the greatest denudation happened in the Paleogene due to records of clastic deposition in sedimentary basins. Some of these sedimentary basins include the North Sea Basin and the Porcupine Basin off the southwest coast of Ireland. It has also been argued that Paleogene denudation was mainly caused by magmatic underplating. Effects of magmatic underplating: a case study Studies have been done on the phenomenon of magmatic underplating in various areas around the world. In northern Italy, the effects of magmatic underplating were studied along a traverse through the Strona-Ceneri Zone and the Ivrea Verbano Zone. The studies included a thermal modeling method which split the cross section up into three different sections: the upper crust, the lower crust, and the upper mantle. The model displayed multiple magmatic intrusions spreading over time, which resulted in the heating up of the lower crust causing metamorphism and anatexis, and even managed to moderately heat up the top of the lower crust. The results also showed that final heating began at the same time as extension in shallower crustal levels, while in deeper parts, extension occurred later than the thermal peak of metamorphism. It was also shown that magmatic underplating during a time period of about thirty million years was strong enough to erase all tectono–metamorphic history in the Ivera Verbano Zone. This information was