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The Floor Boards:

The Floor Boards Old original boards have been painted a powder blue to make a pretty but practical floor. You can buy specialist Floor paints in lots of colours the Floor boardsse days, or simply apply a couple of coats of emulsion the Floor boardsn seal with a tough acrylic varnish. Just remember that any pale Floor shows up marks and crumbs easily, so will need more attention than dark boards would do.

• Metal rule, Stanley knife, pencil • Paint or stain, paint brush, felt pen • Clear polyurethane varnish, matte or satin Q Work on eithe Floor boardsr hardboard or viny has been glued to the Floor boards floor. Mark oul width of Floor board you want with a Using a long metal rule, run down thi with a Stanley Knife to score and mar boards. Q Paint the Floor boards boards with your choser colour or stain.

See Also Common Floor Covering:

Carpet is perhaps the most common Floor covering in homes. It comfortable to walk over and sit on, and can transform any inte instantly. Made from wool or synthetic fibers, or a mixture of th two, carpet is available in a vast range of thicknesses, patterns, colors, textures, and cost. Its durability as a Floor covering depe on quality and the wear it is subjected to.

Whether you plan to lay a new Floor covering or to make a decorative feature of an exposed floor, careful repair and preparation are vital. The Floor should be as level as possible, clean, dry, and smooth. Smoothness is important, since any projections will quickly ruin a covering.


On The Other Hand See Ocean Floor That:

This out¬ward movement could push continental blocks apart or push previous ocean Floor rocks be¬neath the continents, which would explain the comparatively young age of the rocks on the ocean floor. In the Pacific Ocean, for example, the new ocean Floor seems to spread outward from a great ridge known as the East Pacific Rise. As the new Floor moves outward, the older seabed ahead of it should be forced downward into the deep trenches that ring the Pacific Ocean.

Assuming that the newly forming crust at oceanic ridges picked up the prevailing polarity signal of the earth's magnetic field, the result over a long period of time would be strips of ocean Floor that were alternately normally and reversely magnetized. The correspondence between the patterns on the ocean Floor and the known history of the earth's magnetic field is too remarkable to be due to chance [4].
 
 

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