When rock changes into metamorphic rock, its appearance, texture, crystal structure, and mineral content change.
the alignment of a mineral structure
By definition, a mineral must have a definite crystalline structure. Calcite has this. Glass is amorphous, meaning it does not have such a structure.
No. Coal is not a mineral for two reasons: it lacks a crystal structure and it is organic.
Hardness, resistance to weathering, texture, mineral composition, color, and porosity.
Chemical weathering alters the internal structure of minerals by removing or adding elements through processes like dissolution, hydration, oxidation, and hydrolysis. This changes the mineral composition and may lead to the formation of new minerals.
The property least likely to be affected by weathering of a mineral is its crystal structure. While weathering can alter other characteristics such as color, hardness, and luster due to physical or chemical changes, the fundamental arrangement of atoms in the crystal lattice remains largely intact unless the mineral is completely broken down. This stability in crystal structure allows the mineral to retain its identity despite surface alterations.
Changes in the appearance structure and composition of a rock can occur due to weathering, erosion, and metamorphism. Weathering can break down the rock into smaller pieces, while erosion can transport these pieces to new locations. Metamorphism can alter the mineral composition and structure of the rock through heat and pressure, resulting in the formation of new minerals and textures.
yes
Physical weathering is caused by mechanical forces such as temperature changes, frost wedging, and abrasion, while chemical weathering involves the breakdown of rock through chemical reactions like oxidation and hydrolysis. Physical weathering does not change the chemical composition of the rock, whereas chemical weathering alters the mineral structure.
The internal atomic structure of a mineral most likely determines its physical and chemical properties, such as hardness, color, cleavage, and crystal shape. It also influences how the mineral interacts with its environment and how it behaves in different conditions.
The internal structure of a mineral, characterized by its crystal lattice arrangement and chemical composition, directly influences its external appearance, including color, luster, and shape. For instance, the symmetry and bonding of atoms within a mineral determine its crystal form, which manifests as distinct geometric shapes on the outside. Additionally, impurities and defects in the internal structure can affect color and transparency, further impacting how the mineral is perceived visually. Therefore, understanding a mineral's internal structure is key to explaining its external characteristics.
Chemical weathering changes the mineral composition of rocks by altering the chemical composition of minerals through processes like hydration, oxidation, and dissolution. This can result in the breakdown of minerals and the formation of new minerals.
The internal arrangement of atoms.
Amber is not a mineral, because it has an organic origin and amorphous structure (no orderly internal arrangement of atoms).
Physical weathering is a type of weathering that does not involve any chemical changes to the rock or mineral. It occurs through processes like freezing and thawing, which break down rocks into smaller pieces without altering their composition.
Quartz is a mineral that is highly resistant to chemical weathering. Marble is a mineral that is more susceptible to chemical weathering.