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Learn about The best places for detecting metals and gold

Learn about The best places for detecting metals and gold

Gold

Many people seek to search for gold, which is the most important metal that is searched around the world, as it is a hobby for some and a profession for others. Gold is one of the most famous metals and a desire to own by people, whether for the purpose of trading, and the reason for this is due to the stability of its price in the global markets when buying and selling. Gold is still considered the most stable and widely used monetary base at the International Monetary Fund and the Bank for International Settlements. Gold is also widely used in making precious women’s jewelry due to its high value and its striking yellow color. It was also used by ancient civilizations in making jewelry for kings, the most famous of which is the mask of the pharaoh Tutankhamun, which is a masterpiece made of pure gold.

 

Metals

They are solid compounds that arise as a result of geological processes, and are studied within a specialized science known as mineralogy. Because of the importance of minerals, it was classified as the third kingdom in the natural world next to animals and plants, as Carolus Linnaeus classified it in this way. Metals differ among themselves in terms of color, transparency, and luster, and this affects their material and moral value to humans, and in view of this, the person strives to reveal the whereabouts of the precious ones; Such as gold, for example, or to protect itself by detecting the presence of weapons or mines that damage it and to get rid of them before it is too late.

 

Forms of the presence of minerals in nature:

We know where the minerals are and how they originated. The question now is: does it exist alone or does it exist in mixed groups? Are these groups cohesive with each other or loose? What is the resulting form of these groups and natural mixtures?

In order to answer these questions, it is necessary to get acquainted with some scientific terms related to minerals, namely: minerals, mineral ores, mineral deposits.

Minerals are all materials extracted from the earth’s interior and consist of homogeneous chemical compounds, most of which were formed as a result of the fusion of natural elements.

As for mineral ores, they are: largely homogeneous materials consisting of metal components that can be extracted from ores by purification or smelting according to the nature of the ores. From this definition we note that mineral ores refer to metallic minerals such as iron and copper without non-metallic minerals such as sulfur and phosphate.

Mineral deposits are defined as: parts of the earth’s crust that contain one or more minerals that can be exploited on an economic level due to the quality of their properties and their availability in quantities that enable them to be exploited on a large scale. Man has been able to discover a large number of minerals exceeding two thousand, and these minerals constitute the various elements that make up the earth’s crust.

There are different forms in which minerals are found in the earth’s crust by metal detectors, according to the geological conditions during which they were formed. These forms can be identified as follows:

  • Veins:

The mineral may be found in the form of veins permeating the rocks, in the areas where its minerals were concentrated at a later time to form the rocks.

 

  • Minerals concentrated in the rock formation:

The minerals in this case are part of the rocks, as they were within the magma before it cooled or solidified, so they formed independent parts of the rocks even though it was inside them. It occurs when some mineral elements mix with an alkaline or acidic formation in the rocks. Examples include diamond, platinum and nickel, which are minerals found in alkaline rocks, in addition to tungsten and tin, which are minerals found in acidic rocks.

 

  • Layered materials:

Some minerals are concentrated in the form of horizontal layers rather than in the form of veins. Some of these mineral layers may be formed by direct deposition of mineral elements in the bottoms of water bodies, whether lakes or seas, such as some iron ores. Others may form from these mineral layers as a result of the precipitation factor by evaporation from shallow water bodies, as is the case for gypsum ores and potash salts.

 

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