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Environments


Street In Costa do Castelo find other viewpoints with special environments, especially the Chapitô, a single space. School of Circus Arts, bar, café, terrace and restaurant, combined to create a unique, diverse, beautiful and spacious.
Photo: MyField

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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.

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S. Castillo Jorge



Finally, go to the Castle of S. Jorge, where he began the history of the city. This is one of the most visited monuments in the city, not only for its historical and cultural importance, but also by the magnificent views over Lisbon. We found a couple, children and youth, seniors, families and tourists in a friendly atmosphere that crosses centuries and centuries of history.
Photos: Andy54321 and The Dulcinea

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The Shoe orma

As I told you in the previous chapter, my trip to the island of El Hierro were primarily intended to map the orientation of the dikes main island, and the result is the image on the right. As you can see do not seem too, must take into account that only interest the guidelines as a whole group of them is represented by one that represents them all. In the southern tip of the island (very eroded) are not visible levee so I've included a map of the island of La Palma with the guidelines I've listed so far and complete the missing iron.

The photograph top left shows a close up of the end of the test I did with the laser, I've uploaded, because of a simple bright lines that are seen in the image, this was the first major surprise at the direction of dikes, I found on the island. But here is the top right image, it is represented to the island of iron in the left side represents the wave front and its progress as the construction of Huygens and on the right side of radius vector, the latter match the address with the levees in the plane that I made on the island of iron.

As you can see the bright lines of the image on the left (the laser) follow the same pattern as inclining toward the center of the light tip to overlap in the center with the same direction.

in the picture below you can see how the direction of the levees is leaning right and left of the southern tip of the island to take the direction of the southern tip of the island as in laser light and is explained on the right side of the photograph of Iron.

finally pay attention to the left of the photo upper right which represents the construction of Huygens on the wave that propagates in the interior of the island, the direction of the vectors and therefore radio of dykes is inferred from of the tangents to the spherical waves that arise Huygens building house one of the wavefront, since these carry the energy of the wavefront-radiovectores levees (which are nothing more than areas in which light energy is expressed as burst pressure in the rock) are at points that are touched two secondary waves in the right direction, these directions being tangent to these secondary fronts that match the radiovectores (s that laser light lines and address of the levees).

Well this is also the cause of the sporadic existence of dikes perpendicular to the generals, it happens that in areas with high density of dykes receive one or at most two perpendicular to them, this happens for example in front of the entrance to the Parador Hierro National among a group of about 25 or 30 levees seen a perpendicular the rest, the rock stiffened by compression of the main wavefront sporadically breaking efforts to fracture under lesser amount that the radiovectores from carrying the main effort.

and finish for today with a final example of compression waves are common in nature u throw a stone in the sand on the beach, the shows, (the sand is sprinkled along radial lines) even better if you can disponeis a telescope have a look at lunar craters shock waves produced by the asteroid impact that led to clearly manifest in the form of rays that emerge from the crater.

enough for today In the coming days I will write about the why of the rounded shape of Gran Canaria and La Gomera or relationship between the laws of optics of Descartes and the rise of volcanic magma, but that is another day.

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Viewpoints


If we keep going up, without fear of tiring as the discoveries keep us wide awake and eager to see Moreover, we find the viewpoints of Santa Lucia and Portas do Sol
Photo: Vic Lic

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To test my idea I've used a laser light passing through the slot a few millimeters consists of two boxes of matches, light travels through waves, the waves spread through the slot as shown in the picture. The first thing you notice is that the typical shape of such islands is due to the natural propagation of waves through the ranura.He drawn a thin line blue line on the image, the line marking the brightest areas of the image as seen following the star pattern (three arms spaced 120 °) characteristic of islands as you can think Palma.Pero said so far seems to have no connection with the appearance of volcanoes on the island following a pattern with a visible order, at this point, and the idea of \u200b\u200bsolving the problem once and travel (this 2 months ago, the neighbor island of El Hierro, considering that being an island of star structure but younger than the Palm it would follow the trail of the wave propagating inside with ease, as well finally was still, despite my initial success in the 3 or 4 days of walks that led me make a map of the orientation of the dikes on the small island I found two surprises. To understand the next chapter, we must consider the levees are hyperbolic tangent lines wavefront allowing further propagation of the island, but that I leave for later

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A case in point.

This is Palm Island. On it I have drawn the wavefront and how it develops within the isla.Pero to understand because of this picture first dive we surface in the theory of Huygens.

The top right image represents the "construction of Huygens' to the wave front. When I proposed the theory to a physicist friend told me it could be a resonance of the ocean floor north of the island (something like a pitch capable of fracturing the seafloor of the island) the idea was good but the reality seemed to take me to another conclusion, everything happened as if the main wave arriving at a traverse slot and spread to the other side (only the slot in this case is a bathymetric low in the manner explained next article

anteriormente.hasta

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And

reach Canary

Here is a map of the Canary Islands which indicates the local direction of the wavefront arriving Canaries. The first thing that caught my attention is that the islands of La Gomera and Gran Canaria are not directly the wave front, will talk about later. The other fact that worried me is why the energy carried by the front wave (from the dorsal growth of up to hawks as you comment)., is evicted and precisely where it does not elsewhere resulting volcanoes in those other places.
I was hard to find, in fact the first name he gave to the book was "wave theory of compression of bathymetric low to explain the origin of intraplate island" the secret and the explanation is found in low bathymetric As is known ocean depth decreases as we approach the continent this fall in depth to not be constant everywhere leads to real underwater mountains (that's the lower bathymetric) the wavefront hence the energy discharged starting the volcanic process.
In the picture above the island top left is the Palm Island, la elegiremos como modelo para explicar el siguiente paso se trata de una isla formada por tres brazos principales (no voy a dar el nombre que utilizan los vulcanólogos en ingles a estas estructuras en Canarias las llamamos dorsales) estos tres brazos separados por 120º entre ellos (es la conocida como estructura en estrella) esta presente en tres islas del archipiélago Canario el hierro Tenerife y la Palma por lo que las explicaciones son validas para todas ellas .

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Primero fue la idea pero ¿Cuál fue la idea?

Como todos sabemos la teoría de la deriva continental , se apoya en la expansión del océano atlántico a partir del growth on the seafloor, this fact takes place in mid-ocean ridge from material provided from within the planeta.En the picture we can see the ocean ridge. To the west of the ridge seafloor growth displaces towards America west. But what really caught my attention was the ocean floor east of the ridge, first that canary is there, but also by the fact that the Euro-African plate does not move, this important observation led me to the next question what if the ocean floor increases, and this is a proven fact, if Africa does not move happens with the pressure generated by this growth?
This question and the observation that the volcanic islands of the Atlantic are on our side of the ocean brought me to the following explanation.
In the drawing of the dorsal growth occurs in the direction indicated by arrows I have explained what happens on either side of her, the issue is that increased pressure on the ocean floor (not moving) causes fracture the bark at certain points giving rise to oceanic islands, the solution I propose is to interpret the increase of pressure as a wave that spreads from the dorsal to the mainland and with that idea I'm doing this book.
The address of that growth (from now on compression waves) corresponds to the Canary Islands Azores Islands and is approximately 25 ° to Ecuador.

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the beginning was the idea.

A book about volcanology development takes time, on this blog I summarize in a few years of traveling steps Canary Islands, hours of walking and searching, rather than reading books on the subject, and of course what is left.

Finally, as I said, after much thought I decided to gather ideas in a book that had accumulated over years of observation Of this seven years ago, needless to say not as easy as I expected. And that is one thing to have an idea and quite another to translate it in an understandable way to others.

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Cathedral


As we began to climb, we find the most popular Portuguese saints, San Antonio, in a small restored statue in a church with her name and the Museum Antonian. This popular saint draws apology love. Then we find the Cathedral (XIII century), a true monument, whose grandeur and austerity make us stop and get to be surprised.
Photo: kjay.rm

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El Tranvía


The tram is one of the most famous and typical transport in Lisbon. Travel it is to enter into an imaginary past, but also in the present. You can go by tram to Alfama, but a walk along the slope is also quite attractive. Rising from the Baixa, find typical streets, alleys and special viewpoints.
Photo: e2

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Liberty Avenue


Discover, above the Rossio, the Avenida da Liberdade. A walk for which he was in the nineteenth century, the "Public Tour" of the city and where elites gathered to walk nonchalantly. Today in the Avenue are the big brand stores, where they shop most cosmopolitan and international city.
Photo:

scalleja