Magma swingt stream. We infer that the WMR is a remnant melt-storage pocket left behind as the MMR moved eastward relative to the overlying caldera, and cooling and crystallization of magma in this pocket contributes to forming crust beneath the west caldera wall.
| Intereses | Profesión | Hobby |
|---|---|---|
| Leer | Doctor | Bailar |
| Cocinar | Profesor | Pintar |
| Leer | Doctor | Bailar |
Melt to mush variations in crustal magma properties along the ridge crest at the southern East Pacific Rise. Shear attenuation beneath the Juan de Fuca plate: Implications for mantle flow and dehydration.
| Nombre | Edad | Ciudad |
|---|---|---|
| Damita | 27 | Murcia |
| Natalina | 23 | Gijón |
| Xiomara | 21 | La Laguna |
This is consistent with strong amplitudes of coincident seismic reflections, indicating relatively high melt fraction in the upper MMR
This also agrees with the seafloor morphology of Axial Seamount, where the western shoulder is much wider, shallower, and thicker than the eastern one Figs. Girls Just Wanna Have Boys.