How Long Does Robxin Stay In Your Uruin

The new gravitational Valles valley

In the picture below (Figure 1) can be seen as the wave front from the oceanic rift reaches the island of La Palma fault ravine ravine anxieties of lime is the tangent to the wavefront (red line image) is the line where most, is the energy carried by the compression wave, this is the cause of the failure itself.

As we have already seen the collapse of the western flank of the island that gave rise to the valley of Aridane caused the displacement of this wave front to the south resulting in a new fault current training and extension anomalous of the island to the south, anomalous that these islands have a size set by the frequency of the compression wave (determined by the growth of the Atlantic Ridge) and the width of the north of the island, it is as if the island Palma was double, an island north to the crater stew fails rowing and another from there to fuencaliente in the south.
In the next picture (Figure 2) can be cut into the crater of the stew made to build the ring S / C de la Palma, as can be seen that the fracture is caused by the wave front moved south (second red line) on the south side, left, has risen about 4 meters from north (this increase is the result of thrust of the wavefront on the tripod 2 centered at the peak virigoyo is the same phenomenon that produces the elevation of the bottom of the Caldera and his rock pillow, but now the phenomenon is repeated in the new structure facilitates new elevation trípode.La sinking of new valley from this flaw because the rise, as seen in picture 2, the valley tends to discard the existence of one's fault then the collapse favors lifting the entire structure by the weight loss it is and this again favors the collapse ...

we can see that the sinking of the valley is the fault Aridane 1 to the boiler also the new valley, whose formation can be deduced by the incipient arc Bonelli eruption appeared in the San Juan in 1949 follows the path of failure 2 until it intersects with the arc.
I have spoken before of the east-west symmetry of the triangular islands, as we also repeated the structure to the south.
'll go into more detail in a future installment of this blog. While in depth at the origin of volcanism in the blog http://causasdelvulcanismo.blogspot.com/

Promo For Sprint Ringtones

Tejeda in the Sierra de Peña Mayor 2. Bimonthly.

This second visit to the Sierra de Peña Mayor beginning at a place called Fayacaba Bimenes the council, aims to go through the funeral Pozu, climb the Pico Trigueiros, and continue along the entire ridge from Garami Peak, who was on where it was at the previous visit.

-0-0-0-0-0-0-0-0-0-0-0-0-0-0-0-0-0-0-0-0-0-0 - 0-0-0-0-0-0-0-0-0-0-0-0-0-0-0 -

Road to the top of the ridge, we encounter the first puck of some importance, is in meadow area.

this infamous place known as "Pozu funeral" is another reason for the trip of the day, the place is creepy but its history has a puck in the mouth itself Well, it might be a mute witness to the barbarity committed there.

Collado Down the Peak Trigueiros sores did we encounter the first significant yews of the day, it seems that the day will be productive.

The hill that leads to mass Pico yew Trigueiros becomes more apparent, and its importance increases.

El Pico Trigueiros es nuestro destino montañero de la jornada, su cima situada a 1.294 metros es un lugar ideal para hacer un alto reparador en el camino, y al propio tiempo disfrutar del paisaje y de la observación de los abundantes tejos del lugar.

Ascendemos hacía la cima del Pico El Texu, en su vertiente este se aprecia una importante mancha de tejos.

After reaching the Pico El Texu, after leaving behind accelerate the passage way to the Pico Garami, between the two peaks are abundance of yew on the east slope.

Garami Peak of 1,256 meters was the limit our previous visit to the Sierra de Peña Mayor, so we continued along the ridge along the mountain road to the Pico de Peña Mayor, the yews that we see in the previous visit are realized, and we see that our desire to return to the site made sense.

behind us and we Garami Peak road to the Pico Peña Mayor, the path is good with plenty of vegetation and many yews.

Before reaching the peak of Peña Mayor must go through the Pass of Coballa, where the presence of yews is the general tone.

Again Peak spotted Peña Mayor of 1,156 meters, the abundance of yew trees is evident, many of them are at least centuries, and the sight of his observation is impressive.

Shortly before starting the descent from this vantage point we spotted a place called "Les Praeres" is a mayeu with two impressive yew.

On a steep descent we turn away from Pico de Peña Mayor, we are trying to reach the track that will take us to Fayacaba.

Having taken the path that will lead to Fayacaba, we with a series of cabins, most of them converted to housing, many with his "red keel, which makes us think that the future is almost assured.