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The Quran and Mountains: Difference between revisions
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→Alleged function as pegs
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[[File:TectonicSlabs.png|alt=|thumb|425x425px|center|Three-dimensional cross section beneath the European Alps showing attached and detached parts of a lithosphere slab based on tomographic profiles by M. R. Handy et. al. (2021)<ref>Fig. 11 in Handy, M. R., Schmid, S. M., Paffrath, M., Friederich, W., and the AlpArray Working Group: [https://se.copernicus.org/articles/12/2633/2021/ Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography], Solid Earth, 12, 2633–2669, https://doi.org/10.5194/se-12-2633-2021, 2021</ref><BR />Subducted slabs are far more significant downward protrusions than the crustal thickening which occurs beneath some mountain ranges.]] | [[File:TectonicSlabs.png|alt=|thumb|425x425px|center|Three-dimensional cross section beneath the European Alps showing attached and detached parts of a lithosphere slab based on tomographic profiles by M. R. Handy et. al. (2021)<ref>Fig. 11 in Handy, M. R., Schmid, S. M., Paffrath, M., Friederich, W., and the AlpArray Working Group: [https://se.copernicus.org/articles/12/2633/2021/ Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography], Solid Earth, 12, 2633–2669, https://doi.org/10.5194/se-12-2633-2021, 2021</ref><BR />Subducted slabs are far more significant downward protrusions than the crustal thickening which occurs beneath some mountain ranges.]] | ||
[[File:Craton-keel.png|alt=|thumb|425x425px|center|Dynamic model of craton keel formation (fig. 5 in Perchuk et al. (2020) ''Building cratonic keels in Precambrian plate tectonics''<ref name="Perchuk2021"/><BR />These too are much larger downward protrusions than the crustal thickening which occurs | [[File:Craton-keel.png|alt=|thumb|425x425px|center|Dynamic model of craton keel formation (fig. 5 in Perchuk et al. (2020) ''Building cratonic keels in Precambrian plate tectonics''<ref name="Perchuk2021"/><BR />These too are much larger downward protrusions than the crustal thickening which occurs during any mountain formation process.]] | ||
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