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When the object has to be painted with complex shapes or sizes outside the standard decorator is forced to real changes in the tip of the brush ...

If painting a plate is not particularly difficult, even for a beginner, the situation becomes more complicated when you are ready to decorate a vase , especially if large or a small box from edges flat or even porcelain plates for jewelry: all objects that can not handle so easily !
We see then how you can cover even these parts "difficult" so as to make it easier for decoration.

For vessels and, in general, for all objects cables and the trick there is in ' challenge from within rather than outside the piece, putting his hand used to support directly into the jar if this is medium size, or with the help of a support thread in the in improvised by whether the vessel is smaller: we could use a spoon resulted in the correct thickness with a few laps of Scottex.

pots large become too heavy to be supported by the hand : in these cases should use the Torniella or, better yet, turning to those used as support media for television sets that have a thickness of few inches and allow to limit the height of the object is already high.

And if you can work in difficult vertical arm in the air can used to support : some large book stacked vessels may be sufficient for medium-high, while the more bulky maybe just look around to discover that you already have something suitable in the home: a can of detergent, an umbrella a folding beach chair ..... are some of the props, which I happened to improvise!

purists decoration already horrified but they will be formalized ..... because if we found a convenient and practical solution to the problem?! ;-)

© Radaelli-Ross 17:07:06

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Buona visione.

Matina Giovanni

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La Roccia

Per roccia si intende un aggregato naturale di minerali cristallini e/o amorfi, particelle e solidi di vario tipo; le rocce sono sostanze non esprimibili con una formula chimica e generalmente formano masse ben individuabili.
Tipologie
A seconda del processo che dà loro origine le rocce vengono distinte in tre grandi categorie: The
magmatic rocks are igneous rocks also known as generated by cooling of magma, a molten silicate mass containing volatile elements (water, carbon dioxide, acids, hydrogen, etc ...) giving it fluidity and speed up chemical reactions. These rocks are in turn subdivided, depending on the speed and location of the cooling of magma, in plutonic or intrusive igneous rocks, extrusive or volcanic, or ipoabissali filoniane: the first formed in the earth's crust or in part highest mantle and are characterized by a slow cooling promotes the growth of crystals in them (about 150 thousand years), typical of such rocks are granite and quartz-diorite, but the latter are formed after an eruption or a lava flow and therefore undergo a rapid cooling (about a year) that "freezes "Part of the rock in an amorphous state. They are composed of microcrystalline bottom paste, and their structure is glass. Examples are basalt the porphyry and pumice. Then there are the rocks or filoniane ipoabissali, which solidified below the earth's surface, but in small cavities, have a fast enough cooling. Igneous rocks constitute the large majority of the crust and mantle. Examples are the basalt, the granite the diorite. The
sedimentary rocks are the rocks generated sedimentation of debris, inorganic, organic and mineral salts, consolidated by the subsequent or simultaneous deposition of a cementing substance. This is, in essence, lithified ancient sediments as a result of stages of weathering, erosion, transportation and sedimentation. They are the most common rocks on Earth's surface because they cover more than 80% of the land. Examples are the ' sandstone, the limestone the dolomite. The
metamorphic rocks are sedimentary or igneous rocks that have been portate in condizioni di ( pressione e temperatura ) diverse da quelle presenti al momento della litificazione della roccia. In seguito a questi cambiamenti la roccia subisce trasformazioni chimiche e fisiche che ne alterano ad esempio la composizione mineralogica . Alcuni esempi sono l'alabastro e il marmo.
Regole fondamentali
Quando si studiano le rocce, sono tre le regole fondamentali da tenere a mente:
Il principio di Lloyd , cioè le rocce si formano oggi con le stesse modalità con cui si sono formate in passato: temperatura, pressione, acqua, ossigeno e anidride carbonica agiscono sempre nello stesso modo.
Rocce di diversa origine e dalle diverse caratteristiche may be in close contact.
The nature of a rock depends not only on its origin, but also the circumstances in which it comes into being.

GRAMAGLIA EMANUELE

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Le rocce

rocks
To Rock means a natural aggregate of mineral crystalline or amorphous, and solid particles of various kinds, the rocks are not expressible substances with a chemical formula identifiable and generally well-formed masses.

rock types
Depending on the process that gives them the source rocks are divided into three broad categories:

• 
  The magmatic rocks are igneous rocks also known as generated by cooling of magma , a mass of molten silicate containing volatile elements: water, carbon dioxide, acids, hydrogen, etc ...) giving it fluidity and speed up chemical reactions. These rocks are in turn subdivided, depending on the speed and location of the cooling of magma, in plutonic or intrusive igneous rocks, extrusive or volcanic, or ipoabissali filoniane: the first formed in the earth's crust or in part highest mantle and are characterized by a slow cooling promotes the growth of crystals in them (about 150,000 years), typical of such rocks are granite and quartz-diorite, and the latter instead formed after an eruption or a lava flow and therefore undergo a rapid cooling (about a year) that "freezes" the rock in a state amorphous. They are composed of microcrystalline bottom paste, and their structure is glass. Examples are basalt the porphyry and pumice. Then there are the rocks or filoniane ipoabissali, which solidified below the earth's surface, but in small cavities, have a fast enough cooling. Igneous rocks constitute the large majority of the crust and mantle. Examples are the basalt, the granite the diorite.

• 
  The sedimentary rocks were generated for sedimentation of debris, inorganic, organic and mineral salts, consolidated the subsequent or simultaneous deposition of a cementing substance. This is, in essence, lithified ancient sediments as a result of stages of weathering, erosion, transportation and sedimentation. They are the most common rocks on Earth's surface because they cover more than 80% of the land. Examples are the ' sandstone, the limestone , the dolomite

• The metamorphic rocks are sedimentary or igneous rocks that have been made in terms of ( pressure and temperature ) different from those present for the lithification of the rock. Following these changes, the rock undergoes chemical and physical transformations that alter the mineralogical composition, for example. Examples include, alabaster and marble.

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