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What is VMS? Assemblages of mostly sulfide minerals that develop on the seafloor at locations of concentrated hydrothermal discharge, relates to a kind of ore deposit that’s mined from existing oceanic crust formed underwater are Volcanogenic Massive Sulfides (VMS) Deposit. ...
Geology 101 is the study of the Earth and its materials, structures, processes, and history. It is a broad field that encompasses many different disciplines, including mineralogy, petrology, paleontology, and geophysics. Geologists study the Earth’s physical features, including its rocks, ...
Geologic mapping is a crucial process in the field of geology, which involves creating a detailed representation of the Earth’s surface based on the study of its rocks, minerals, and physical features. This article will provide a comprehensive overview of ...
Geology is the scientific study of the all constituents of planets, their internal and external forms and processes. More precisely, it is the study of nature, structure and history of the planet. Earth is the home to all life, well ...
All of the important processes of metamorphism that we are familiar with can be directly related to geological processes caused by plate tectonics. The relationships between plate tectonics and metamorphism are summarized in Figure. Most regional metamorphism takes place within continental ...
A landslide is a geological phenomenon that occurs when soil, rocks, and debris suddenly move down a slope due to various factors such as gravity, erosion, seismic activity, or human activity. Landslides can cause significant damage to buildings, infrastructure, and ...
Exploring the World of Geoscience: Branches, Importance, and the Life of a Geoscientist Geoscience is a multidisciplinary field that encompasses the study of Earth’s physical processes, materials, and history. It is the foundation for understanding our planet and its natural ...
Porosity Definition Porosity refers to the amount of empty space or voids within a material or substance. It is often expressed as a percentage of the total volume of the material, with the remaining percentage being occupied by the solid ...
The law of superposition is a fundamental principle in geology and archaeology that states that in a sequence of undisturbed sedimentary rocks or archaeological layers, the oldest layers are at the bottom, and the youngest layers are at the top. ...
Skarn Deposits: Unraveling the Geological Marvel Skarn deposits, also known as skarns, represent a fascinating geological phenomenon formed through the interaction of hot fluids from intrusive igneous bodies with carbonate-rich sedimentary rocks. In this comprehensive guide, we’ll explore the various ...
What the meaning of Bauxite ? Bauxite is the most important aluminum ore. This type of rock consists mainly of the minerals gypsite Al(OH)3, bohemite γ-AlO(OH), anddiaspore α-AlO(OH) in a mixture that usually includes iron oxide goethite,hematite,the clay mineral kaolin, ...
Soil classification tests are methods of determining the physical and engineering properties of soils, such as moisture content, specific gravity, grain size distribution, Atterberg limits, and shear strength. These tests are important for geotechnical design and construction, as they help ...
In geology, a vesicle is a small cavity or void in a rock that is typically formed by the entrapment of gas or other volatile substances during the cooling and solidification of molten rock, such as lava or magma. Vesicles are common features in certain types of volcanic and igneous rocks, and theyRead more
In geology, a vesicle is a small cavity or void in a rock that is typically formed by the entrapment of gas or other volatile substances during the cooling and solidification of molten rock, such as lava or magma. Vesicles are common features in certain types of volcanic and igneous rocks, and they often leave behind distinctive voids or cavities after the rock has solidified.
Key characteristics of vesicles in geology include:
1. **Formation in Volcanic Rocks:** Vesicles are most commonly associated with volcanic rocks, such as basalt and scoria. When magma erupts onto the Earth’s surface as lava, the rapid decrease in pressure allows dissolved gases (primarily water vapor, carbon dioxide, and sulfur dioxide) to come out of solution and form bubbles or vesicles in the molten rock.
2. **Size and Shape:** Vesicles can vary in size, from tiny microscopic voids to larger cavities that are visible to the naked eye. They can have irregular shapes, and their distribution within a rock can be relatively uniform or clustered.
3. **Filling Material:** Vesicles may contain secondary minerals or other materials that have filled the cavities over time. Common filling materials include minerals like quartz, calcite, or zeolites.
4. **Impact on Density:** The presence of vesicles can reduce the density of a rock because they occupy space without adding mass. This can result in a lower specific gravity compared to similar rocks without vesicles.
5. **Identification:** Vesicles can be identified by their typically round or elliptical shapes, and they often have smoother interiors compared to fractures or cracks in rocks. They are a useful feature for distinguishing volcanic rocks and understanding their eruptive history.
6. **Geological Significance:** Vesicles can provide information about the volcanic environment, including the amount of gas dissolved in the magma, the depth of volcanic activity, and the cooling history of the lava or magma.
Vesicles are just one of many features that geologists use to analyze and interpret the origin and history of rocks. They are particularly common in volcanic rocks, where rapid cooling and gas release during eruptions create ideal conditions for vesicle formation.
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