Amphiboles are double chains of silicate units, whereas pyroxenes have only single chains.
Cellulose is made up of multiple glucose units bonded together in a complex structure, which allows for more potential energy storage due to the greater number of bonds that can be broken to release energy. Glucose, on the other hand, is a simple sugar with a single molecule, providing less energy storage potential compared to the complex structure of cellulose.
Starch is a more complex carbohydrate than reducing sugar. Reducing sugars are simple carbohydrates that can reduce other compounds, while starch is a complex carbohydrate made of many sugar units linked together in a more elaborate structure.
Proteins with more than one polypeptide chain have a quaternary structure. This structure is formed by the assembly of multiple polypeptide chains into a functional protein complex. The interactions between the individual polypeptide chains contribute to the overall structure and function of the protein.
Formic acid is more acidic than benzoic acid. This is because formic acid has a simpler molecular structure with a hydrogen atom attached to a carboxyl group, making it easier to release the acidic hydrogen ion compared to benzoic acid, which has a more complex aromatic ring structure.
Polysaccharides contain more glucose units, which means more potential energy can be stored in the form of chemical bonds. This structure allows polysaccharides to be broken down gradually, providing a sustained source of energy for the body. Monosaccharides, on the other hand, supply quick but short-lived bursts of energy due to their simple structure.
Diabase is a mafic, fine-grained igneous rock composed mostly of plagioclase feldspar and pyroxene. Diorite is also an igneous rock, but it is intermediate in composition between mafic and felsic, consisting mainly of plagioclase feldspar and amphibole. The main difference lies in their mineral compositions, with diabase containing more pyroxene and diorite containing more amphibole.
Amphibole and olivine can be differentiated based on their mineral structure and composition. Amphibole is a complex silicate mineral with a double-chain structure, typically containing hydroxyl groups (OH) and exhibiting a range of colors, while olivine is a simple silicate with a single-chain structure, primarily composed of magnesium and iron silicate (Mg, Fe)2SiO4. Additionally, olivine commonly appears green and has a glassy luster, whereas amphibole can exhibit a more varied color palette and often has a more fibrous or prismatic habit. Lastly, amphibole has a lower hardness than olivine, making it easier to scratch.
There are more people in the hierarchical structure then the matrix structure. The matrix structure is more complex than the hierarchical structure
Quartz is a mineral composed of silicon dioxide (SiO₂) and is characterized by its hexagonal crystal structure, hardness, and lack of cleavage. In contrast, pyroxene is a group of silicate minerals that typically contain iron, magnesium, and calcium, displaying a more complex crystal structure and two distinct cleavage directions at approximately 90 degrees. While quartz is commonly found in igneous, metamorphic, and sedimentary rocks, pyroxene is primarily found in mafic and ultramafic igneous rocks. Additionally, quartz is generally transparent to translucent, while pyroxenes are usually opaque and exhibit various colors depending on their composition.
no, Pyroxene is a Mineral not a rock. Rocks are made up of 2 or more minerals
Fractional crystallization of olivine and pyroxene can lead to the formation of a variety of igneous rocks, particularly those in the mafic and ultramafic categories. As these minerals crystallize from a melt, they can deplete the remaining liquid in magnesium and iron, resulting in the formation of more silica-rich minerals like plagioclase and amphibole in later stages. This process can eventually yield rocks such as basalt or gabbro, depending on the extent of crystallization and the composition of the initial melt.
Gabbro is usually made up of minerals such as pyroxene, plagioclase, amphibole and olivine which makes it an intrusive igneous rock.
The quaternary structure is the overall structure of an enzyme complex. This is made of at least two separate polypeptide chains. The 3D structure of one polypeptide is known as the tertiary structure.
More people were working and the economy was thriving
Gabbro has a dull to shiny luster, depending on the mineral composition and how the light reflects off its surface. It typically has a more mafic composition with minerals like pyroxene and amphibole, which can create a dull appearance, but variations in mineral content can lead to some sections of gabbro having a shinier luster.
The disadvantage of the capital structure decision is that it is very complex and expensive. The advantage is that it leads to more company profits.
Instead of nobles and pleasents, a more complex social structure emerged, made up of three classes.