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rising levees

all know the laws of discards optics applied to explain the refraction and reflection of waves. In this article try to explain my theory about the rise of magma through of the different layers of rock that separated from magma terrestre.Este surface, the drilling up Earth's crust, is oscillating, ie a vibration drilling and thus entails an oscillation frequency. This allows the study of his ascent using the laws of discards taken as reference data density of the materials to pass through as data for the index of refraction and cited frequently associated with rising magma as input to solve the equations of discards. . Look at the first photo:

The image above is taken from a farm track near the port of Naos road at the height Rowing Charco Verde. As you can see I've marked in blue the route of the dyke at the bottom ascenso.En dam (just above the blue line) comes with a little inclination around 25 or 30 degrees to reach the first basalt layer is (compact and very dense) is close to normal visibly as you would any ray of light passes from one medium to another lower rate of higher refractive index (see the second picture in which the laser passes from air water with similar slope). After passing this first layer through another basaltic dike formed by volcanic debris located on the former that the dam continues to rise with an angle similar to indicates that the initial intermediate basalt layer is sandwiched between two layers of lower density (something similar happens when light passes through a sheet of glass with parallel faces) in this case volcanic slag .. If you look back into the picture the dam starts now away from the vertical (ie normal) showing that as it rises is becoming less dense layers and light-colored layer (from a crater hydromagmatic to 2 km of the zone) inclines toward the normal dam (is more dense), the layer that follows continues this process, however the following layers cause a progressive departure from the normal which indicates a decrease in the density of materials . pared.La upper third picture is taken from the shanty town of the paddle, we see it dam is diverted to the left to cross a small cinder cone density

emphasize that the levees in their ascent general rule is inclined from magma chamber to the surface in the opposite direction away wavefront (in the Canary Islands from north to south) and from outside the island interior, this is due to less dense materials are found to rise (not only by its constitution, but because they are under less compression than the upper layer) levees also have a tendency to lean to the south by the growth of the oceanic ridge strongly compressed north of the island increasing its density. This can be seen in numerous dams palm, an example is the new summit whose epicenter would be in Santa Cruz de la Palma, while the top appears in the creek area 10 or 15 km to the west, however this apparent anomalies exist to this rule west of the island in the time following the bed of the ravine of the anguish from the beach inland Tazacorte see how the levees are inclined to the interior of the island but at the height of the horses back levees away from the center of the island to enter the boiler levees to lean back into it. That is always away from normal rather well right to the left.
This phenomenon could determine the exact location where the volcano arise, knowing the location of the epicenter, seismic rate of magma ascent and the density of the materials that make up the island.