i think crystal habit is the minerals structure, while cleavage is the patter it breaks into.
Diamonds are hard because of their unique atomic structure, which consists of carbon atoms bonded in a strong, three-dimensional network. This network of bonds makes diamonds extremely resistant to scratching and breaking, giving them their renowned hardness.
Diamonds are formed into crystals with a perfect octahedral crystal habit. Hardness is associated "...with the crystal growth form, which is single-stage..." "The Mohs scale of mineral hardness characterizes the scratch resistance of various minerals through the ability of a harder material to scratch a softer material." All quotes according to Wikipedia research.
The mineral family that tends to form long needlelike crystals is the amphibole group. Examples of minerals in this group include hornblende and tremolite. These minerals are silicate minerals with a double chain structure, which contributes to their characteristic needlelike crystal habit.
Diamond is harder than graphite because of its molecular structure. In diamond, each carbon atom is bonded to four other carbon atoms in a tetrahedral structure, creating a strong and rigid network. This structure allows diamond to form strong covalent bonds, making it extremely hard. In contrast, graphite has a layered structure where each carbon atom is bonded to three others in a hexagonal lattice, with weak van der Waals forces between the layers, leading to its softer nature.
Albert Einstein smoked mostly out of habit and to relieve stress. He started smoking when he was young and struggled with the addiction throughout his life, despite being aware of the health risks.
The crystal habit is the way a mineral grows when it is uninhibited (not interfered with with other minerals or limits on the growing space).
Yes, a mineral can have a prismatic habit without exhibiting cleavage. Prismatic habit refers to the crystal form of a mineral that resembles elongated, prism-like shapes. Cleavage, on the other hand, is the tendency of a mineral to break along specific planes of weakness in its structure. A mineral may grow in a prismatic shape while lacking defined cleavage planes, resulting in a more conchoidal or uneven fracture instead.
types of atoms present in its chemical structure. These properties include hardness, color, luster, cleavage, and crystal habit. The geometric arrangement of the particles within the crystal lattice also affects its physical and optical properties.
Calcite commonly exhibits three notable cleavage planes, which are oriented at approximately 75-degree angles to one another. This characteristic cleavage is a key feature that helps in identifying calcite among other minerals. Additionally, calcite can exhibit a rhombohedral crystal habit due to the arrangement of its atoms. Overall, its cleavage and crystal structure contribute to its unique optical properties.
Yes, a mineral can exhibit a prismatic habit without having any cleavage. Prismatic habit refers to the elongated, column-like shape of the mineral's crystals, which can occur regardless of the internal atomic structure. Cleavage, on the other hand, is the tendency of a mineral to break along specific planes of weakness in its crystal structure. Some minerals may develop a prismatic form due to their growth conditions while lacking cleavable planes, resulting in a fracture instead of cleavage.
Muscovite generally displays a micaceous crystal habit, of thin flexible sheets.
A tabular crystal habit refers to the appearance of a mineral crystal as a somewhat flat, tablet shaped form.
Minerals can be recognized and distinguished based on physical properties such as color, luster, hardness, cleavage or fracture, specific gravity, and crystal habit. These properties can help in identifying different minerals as they each have unique characteristics that can be used for classification.
A habit.
sorry i do not know
The properties you would use to help distinguish one mineral from another are: crystal form and habit, hardness (mohs scale), magnetism, cleavage, streak color, luster, sometimes taste or smell, color can be pretty unreliable.
There are many factors to consider when identifying minerals. However, one factor cannot be used solely to determine the type of mineral. Geologists check for color, streak, hardness, cleavage, specific gravity, and crystal form and mineral habit.