Sign up to join our community!
Lost your password? Please enter your email address. You will receive a link and will create a new password via email.
You must login to ask a question.
Please briefly explain why you feel this question should be reported.
Please briefly explain why you feel this answer should be reported.
Please briefly explain why you feel this user should be reported.
This site uses Akismet to reduce spam. Learn how your comment data is processed.
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, ...
Sand dunes are dynamic landforms created by the wind-driven accumulation of sand. They are typically found in deserts, coastal areas, and even some inland regions. Sand dunes can take on various shapes and sizes, influenced by factors such as wind ...
Placer deposits are natural occurring concentrations of minerals and metals that are found in sedimentary rock formations. These deposits are formed through a series of geological processes that involve the movement, deposition, and alteration of minerals. They are an important ...
Bowen’s series reaction is a model that describes the crystallization of minerals from a magma. It was developed by the American petrologist Norman L. Bowen in the early 1900s. According to the Bowen’s series reaction, minerals crystallize from a cooling ...
In engineering and geology, a fault is a fracture or discontinuity in the Earth’s crust where movement or displacement has occurred. Types of faults Causes of Fault The causes of faults are diverse and depend on the type of fault. ...
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 ...
When we think about tunneling, we often picture massive machines and skilled laborers hard at work underground. While these elements are undoubtedly essential, there’s an unsung hero behind every successful tunneling project: the geologist. In this article, we’ll explore the ...
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 ...
Unveiling the Rich Tapestry of Iron Ore Hematite, a mineral of profound geological significance, stands as one of the most abundant and economically vital iron ores on Earth. Let’s delve into its intricacies, exploring both its physical and chemical properties. ...
Unveiling the Mysteries of Igneous Rocks Introduction: Igneous rocks, born from the fiery depths of the Earth, hold a unique place in the geological tapestry. Formed through the solidification of molten magma or lava, these rocks play a pivotal role ...
Geologists use a wide range of tools and techniques to study the Earth’s physical properties, composition, and structure. Some of the most common tools used by geologists include: Geologists use a variety of specialized tools and equipment to study and ...
Diabase or dolerite is a type of igneous rock that is composed primarily of plagioclase feldspar, pyroxene, and sometimes olivine. Plagioclase feldspar, which is a type of feldspar that contains calcium and sodium, is typically the most abundant mineral in diabase. In some cases, diabase can displayRead more
Diabase or dolerite is a type of igneous rock that is composed primarily of plagioclase feldspar, pyroxene, and sometimes olivine. Plagioclase feldspar, which is a type of feldspar that contains calcium and sodium, is typically the most abundant mineral in diabase.
In some cases, diabase can display white lines or streaks that are composed of plagioclase feldspar. These white lines are commonly referred to as feldspar laths or feldspar porphyroblasts, and they are often visible to the naked eye.
The formation of these white lines is typically the result of a process known as crystal growth or crystallization. When diabase cools and solidifies from a molten state, the plagioclase feldspar crystals grow at different rates, with some crystals growing faster than others. This can lead to the development of large, well-formed feldspar crystals that are visible as white lines within the rock.
The presence of feldspar laths or porphyroblasts in diabase can be useful for geologists in identifying and classifying the rock. It can also provide insights into the conditions under which the rock formed, such as the rate of cooling and the presence of other minerals or substances in the magma
See less