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GEOLOGY HUB Latest Questions

Native metals Native metal is a term used to describe metals discovered in their natural, elemental form – either as an alloy, or in pure form. The list of metals which can occur in native deposits is long, though very few can ...Read more

Native metals

Native metal is a term used to describe metals discovered in their natural, elemental form – either as an alloy, or in pure form.

The list of metals which can occur in native deposits is long, though very few can withstand the natural processes of weathering and oxidization.

Most native metals (including aluminum, arsenic, bismuth, cadmium, chromium, cobalt, iron, lead, mercury, nickel, selenium, tin, titanium, tungsten, and zinc) are highly reactive when exposed to water, light, and other elements of nature – which means they are more likely to occur as small, isolated pockets of reduced ore, or as small flakes or inclusions.

Gold, silver, copper, and platinum are the least reactive of native metals.

This greater capacity for endurance means they are the most likely native metals to be discovered in larger deposits – and their wider availability and occurrence offers a variety of interest to collectors.

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Minerals containing elements of economic value are generally present in all igneous rocks, but the elements may not be concentrated enough to make mining economical. Only in relatively rare circumstances are they in sufficient abundance so that mining is profitable. If the ...Read more

Minerals containing elements of economic value are generally present in all igneous rocks, but the elements may not be concentrated enough to make mining economical.

Only in relatively rare circumstances are they in sufficient abundance so that mining is profitable.

If the minerals are scattered throughout a host rock, but in sufficient amounts to mine profitably, we call the deposit a disseminated deposit.

Disseminated deposits produce most of the world’s diamonds, copper, and molybdenum and also large percentages of the available tin, silver, and mercury.

Often, disseminated ores consist of minerals scattered randomly in a host rock.

Sometimes geological processes concentrate ore minerals in vein deposits consisting of veins that are centimeters to meters thick.

If ore is distributed in many small veins, geologists call the deposit a lode deposit. Vein deposits account for most of the world’s gold and silver mines, and also some copper and lead-zinc mines.

In still other kinds of igneous deposits, ore minerals become concentrated in layer

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Most geologists involved in almost every phase of field geology use geologic maps. For example, petrologists use these maps to determine the location of possible economic resources, such as metal ores, water, or oil. Ceomor· phologists use such maps to ...Read more

Most geologists involved in almost every phase of field geology use geologic maps. For example, petrologists use these maps to determine the location of possible economic resources, such as metal ores, water, or oil. Ceomor· phologists use such maps to detect potential hazards in various areas, such as areas prone to earthquakes, flooding, or landslides. Occasionally, geologic profiles are also provided on these maps to help scientists understand, for example, the rock underlying an area.

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A geologic map is actually a form of topographic map, but in this case it shows the type of sediment or rock outcrops exposed at the Earth’s surface, along with the contour lines. The information on these maps can range ...Read more

A geologic map is actually a form of topographic map, but in this case it shows the type of sediment or rock outcrops exposed at the Earth’s surface, along with the contour lines. The information on these maps can range from the rock type and age to the orientation of rock layers and major (and sometimes minor) geologic features.

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Jade and serpentine are two important types of minerals that have applications in jewelry and ornamental industries. The key difference between jade and serpentine is that jade is comparatively harder and less scratchy, whereas serpentine is softer and scratches more ...Read more

Jade and serpentine are two important types of minerals that have applications in jewelry and ornamental industries. The key difference between jade and serpentine is that jade is comparatively harder and less scratchy, whereas serpentine is softer and scratches more easily than jade. Jade is considered to be more precious and valuable than serpentine.

 

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One major difference between basaltic and granitic magma is their specific mineral contents. Basaltic magma contains between 45 and 55 percent silicon dioxide and is high in magnesium, iron and calcium, while granitic magma contains between 65 and 75 percent ...Read more

One major difference between basaltic and granitic magma is their specific mineral contents. Basaltic magma contains between 45 and 55 percent silicon dioxide and is high in magnesium, iron and calcium, while granitic magma contains between 65 and 75 percent silicon dioxide and only small amounts of those minerals.

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These three igneous rocks pretty much have the same chemistry and mineralogy. The are all black or very dark grey. The main difference between them is the grain size. Basalt is fine grained and Gabbro is course grained. This is ...Read more

These three igneous rocks pretty much have the same chemistry and mineralogy. The are all black or very dark grey. The main difference between them is the grain size. Basalt is fine grained and Gabbro is course grained. This is due to the rate of cooling of the molten magma. Basalt is a volcanic rock that cooled rapidly when erupted from a volcano, so the crystals did not have much time to grow. . Dolerite was intruded into existing rocks as sills and dykes so it was more insulated than basalt and developed larger crystals. Gabbro cooled very slowly in the magma chamber so the crystals had plenty of time to grow.

If you look at basalt closely you will not normally be able to see the crystals with the naked eye, but you might be able to with a hand lens. This tough rock can be seen being used as cobble stones in to streets of Hull’s Old Town and sometimes in the Avenues and Dukeries. It is also used in cemeteries for memorials and takes a high glossy polish; this makes it hard to photograph because you can see the reflection of the camera and photographer! On modern memorials the lettering is often picked out in white or gold; pictures can be etched in using a laser.

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Latest Geology Articles

GEOLOGY HUB Latest Articles

Porphyry Copper Deposits: Formation Processes and Economic Significance

Porphyry copper deposits are among the most significant sources of copper globally, accounting for over 60% of the world’s copper production . 1. Geological Overview a) Geological Background Porphyry copper deposits are typically associated with magmatic arcs related to subduction zones, where an oceanic plate subducts beneath a continental or another oceanic plate. This tectonic […]Table of Contents Toggle 1. Geological Overviewa) Geological Background

Ore-Bearing Hydrothermal Fluids: Key Drivers in Mineral Deposit Formation

Introduction Ore-bearing hydrothermal fluids are one of the most important agents in the formation of mineral deposits. These fluids, which originate from various geological processes, have the ability to dissolve, transport, and deposit metals in economic concentrations. The study of hydrothermal fluids is crucial for understanding ore genesis and guiding mineral exploration. This article provides […]Table of Contents Toggle Introduction1. Sources of Hydrothermal Fluids

How to Identify Gold-Bearing Rocks in the Field: A Geologist’s Guide

Gold has been one of the most sought-after minerals for centuries due to its value and rarity. Prospectors, geologists, and even hobbyists often search for gold-bearing rocks in the field. But how do you identify rocks that contain gold? This guide will provide an in-depth look at the geological features, rock types, and mineral indicators […]Table of Contents Toggle 1. Understanding the Geological Settings of Gold

Alteration in Geology: Types, Processes, and Significance

Introduction Alteration in geology refers to mineralogical, textural, and chemical changes in rocks due to interactions with fluids, temperature variations, and pressure changes. This process occurs in diverse geological settings, including hydrothermal systems, weathering environments, and metamorphic terrains. Understanding alteration is essential in mineral exploration, petrology, geotechnical engineering, and environmental studies. This article explores the […]Table of Contents Toggle IntroductionTypes and Processes of Alteration

Induced Polarization Method in Sulfide Ore Exploration

Introduction The Induced Polarization (IP) method is one of the most effective geophysical techniques used in the exploration of sulfide ore deposits. This method is particularly useful for identifying disseminated sulfide minerals, which are commonly associated with copper (Cu), gold (Au), silver (Ag), zinc (Zn), and lead (Pb) deposits. This article provides a detailed overview […]Table of Contents Toggle Introduction1. Understanding the Induced Polarization ...

Pathfinders for Gold Deposits

Introduction Gold exploration is a complex process that requires a combination of geological knowledge, geochemistry, and geophysical techniques. One of the most effective methods for locating gold deposits is the identification of pathfinder elements and minerals. Pathfinder elements and minerals are geochemical indicators that suggest the presence of gold nearby, even if the gold itself […]Table of Contents Toggle IntroductionWhat Are Pathfinders for Gold Deposits?

The Crucial Role of Structural Control in Hydrothermal Gold Deposits

Introduction Structural control is one of the most significant factors influencing the formation and distribution of hydrothermal gold deposits. Structural geology determines the pathways for mineralizing fluids, the locations of ore deposition, and the overall geometry of gold-bearing zones. Understanding these structural controls is essential for exploration geologists seeking new gold deposits and for mining […]Table of Contents Toggle IntroductionStructural Controls in Hydrothermal Gold Deposits

What is Geology? Defination, Importance, Branches and Facts

Introduction to Geology Geology, derived from the Greek words geo (Earth) and logos (study), is the scientific discipline dedicated to understanding the Earth’s composition, structure, processes, and history. It seeks to answer fundamental questions: How did mountains form? Why do volcanoes erupt? What clues do rocks hold about ancient life? From the atomic structure of […]Table of Contents Toggle Introduction to Geology

Engineering Geological Tests: Purpose, Types, and Applications

Engineering geological tests are critical for assessing the physical, mechanical, and chemical properties of rocks and soils to ensure safe and cost-effective design of infrastructure (e.g., dams, tunnels, foundations). These tests help determine material strength, stability, permeability, and susceptibility to hazards like landslides or subsidence. Below are key tests categorized by their application: 1. Field […]Table of Contents Toggle 1. Field Tests (In-Situ)2. Laboratory Tests

What is sand dunes,Types of Sand Dunes and formation?

Sand Dune Landform: Formation, Types, and Significance Sand dunes are dynamic landforms created by the interaction of wind, sand, and vegetation. These striking natural features are common in deserts, coastal regions, and even in some semi-arid and arid zones. This article explores every aspect of sand dunes, including their formation, types, ecological significance, and role […]Table of Contents Toggle Sand Dune Landform: Formation, Types, and Significance

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