Sedimentary

Summarizing the rocks feldspaticas when for the action of the heat and the extreme cold in way strong rains produce fragmentos microscopical of 0,002 mm, in a lesser ratio that the common one that as already we saw is of 0,005 mm, these adhere to the superficiality that led for the rapids of the water and deposited the edges of the rivers and the lakes the called argiliticos deposits of Tabatinga form as already we saw previously. Argilas thus generated is called secondary, since the primary clay remains in the place where if it originated, which happens for intermediary of the feldspaticas rocks. Therefore very well; already we can have with this a notion sufficiently significant with regard to that type of rock Christ wanted to mention itself in its speech in the sermon of the mount. Being thus, so that let us can finish this study is concentrated in what we will go to conclude now: in an inverse process of litificao (rocky formation) the clay can be changedded into rock sedimentary. Perhaps I know, you I do not know what it is a rock sedimentary, more however you already know what it is a litificao and that its inverse process drift of its rocky spalling. In this way when to know what he is rocky sedimentation we will decipher with some words the enigma of the rock of Christ. What it is therefore a rock sedimentary? The sedimentary rocks are formed from the pressure exerted under particles of sediments loaded and deposited by action of the wind ice or water. As the sediments if accumulate, they go suffering to each time more pressure, if making solid, in a process known for litificao (rocky formation) now it allows me following question it: which they are the places where if can find this call rock sedimentary? It would like before continuing of clarifying to it that the word sediment means ' ' solid material deposited by action of the gravity in the water and ar' '.