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.
The hardness of a diamond is related to the way it was formed because diamonds are formed under high pressure and temperature deep within the Earth's mantle. This process creates a strong and compact crystal lattice structure, resulting in the exceptional hardness of a diamond.
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).
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.
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.
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.
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.
sorry i do not know
A tabular crystal habit refers to a flat, plate-like shape exhibited by certain crystals. These crystals have two dimensions that are much larger than the third, resulting in thin, flattened shapes resembling a plate or tablet. This habit is commonly observed in minerals like mica and barite.
habit