Clay minerals, quarts, feldspar
some minerals are mica, fledspar, and rocks are marble, shale ,slate,granite etc.
Yes, slate was once shale. Shale is a sedimentary rock formed from the compaction of mud and clay, while slate is a metamorphic rock that forms from the metamorphism of shale. The process of metamorphism involves heat and pressure, which transforms the shale into slate by aligning the minerals and creating a foliation (layering) within the rock.
Not in the amounts you would expect from a metal, but surprisingly yes. This is mainly due to the water in the pores, whose conductivity is increased by ions from the minerals in the shale.
Shale rock can be identified by its fine-grained texture and layered appearance, often exhibiting thin, flat sheets or fissility. It typically feels smooth to the touch and may have a dull luster. Shale is composed primarily of clay minerals and can vary in color, commonly appearing in shades of gray, black, or brown. Additionally, it may contain fossils or organic material, indicating its sedimentary origin.
Rocks are aggregates of minerals,thus there is no rock without minerals. Q.E.D
no
Shale typically contains minerals such as clay minerals (like kaolinite, illite, and smectite), quartz, calcite, feldspar, and pyrite. The exact mineral composition can vary based on the specific shale formation.
Shale rock is primarily composed of clay minerals and small particles of other minerals like quartz and calcite. These minerals are compacted together over time to form the distinct layers of shale rock.
Shale is not an element. Shale is a type of sedimentary rock composed of clay-sized particles that have been compacted over time. It is made up of various minerals such as quartz, feldspar, and clay minerals.
== Shale is a sedimentary rock, comprised of lithified mud and clay minerals.
Shale turns into slate through a process called metamorphism, where heat and pressure transform the shale's minerals into new minerals like mica and chlorite. This process also causes the shale's original clay minerals to recrystallize, making it more compact and giving it a foliated texture characteristic of slate.
Shale forms from the compaction of mud or clay sediments, often in quiet water environments such as lakes or deep ocean basins. These sediments are typically rich in fine particles such as clay minerals and organic matter, which bond together to create the layered structure of shale.
Well, sedimentary rock shale has been around for ages.So it would probably be around 150 -200 years old.
Minerals could include clays, feldspars, quartz, micas, and pyrite
The chemical formula of shale is variable, as it is a sedimentary rock composed mainly of clay minerals, quartz, and other minerals. The general formula can be written as (Al,Si)3O10(OH)2, representing the presence of aluminosilicate clay minerals in shale.
Identifying minerals in shale and slate can be difficult because these rocks typically have fine-grained textures that make individual mineral crystals hard to see with the naked eye. Additionally, shale and slate often contain a mix of minerals like clay minerals, quartz, and micas that can be challenging to distinguish without specialized equipment like a microscope or chemical analysis. The high degree of metamorphism in shale and slate can further alter the mineral composition, making identification even more complex.
Shale can sometimes contain magnetic minerals, such as magnetite or hematite, which can make it slightly magnetic. However, the magnetic properties of shale can vary depending on the specific mineral content and geological conditions.