It is also known as silicic acid, a term usually used for its form dissolved in water.

In general, silicic acid reactions are difficult to control.

Silicic acid is created near the ocean's surface, by the process of hydration.

The first of these results is attained by the use of silicic acid.

They can also be used to produce silicic acid fibers by a dry spinning method.

It degrades to silicic acid, which causes no harm to the body.

The area is made up of scoria cone and silicic dome fields.

This points at the same time to the healing forces which silicic acid can unfold in the human organism.

Some of the material in the sandstones originated from silicic volcanoes far to the west.

All this is dependent upon a correct distribution of the activities of silicic acid.

In addition, contact with eyes may form silicic acid with resultant irritation.

The silicic acid, when weathered, forms black streaks, which give the rock its characteristic appearance.

The amount of silica that constitutes a silicic rock is usually put at at least 65 percent.

Rocks high in silica produce silicic acid as a weathering product.

This may be done by administering silicic acid, which always strengthens the inherent forces against sensitivity.

It is thought that fossils were pervaded with silicic acid due to this volcanic activity.

Choanoflagellate biosilicification requires the concentration of silicic acid within the cell.

The silicic acid has a dual function.

We are then dealing with an accumulation of the silicic acid activity in the neighbourhood of this organ.

A 7 km2 silicic lava flow lies on the saddle between the volcano and Acamarachi.

Thin silicic ash beds are also present.

Like other silanols, silicic acid is a weak acid.

Most ignimbrites are silicic, with generally over 65% SiO.

It is home to the Idavada Volcanics formation of silicic rocks.

The gels used are usually gelatin, agar or silicic acid gel.