Textural maturity refers to the development of a food's texture as it ripens or matures. This includes changes in firmness, moisture content, and overall mouthfeel of the food as it reaches its optimal eating quality. Textural maturity is often associated with fruits, vegetables, and cheeses that improve in texture as they ripen.
I think you might be referring to what is called textural maturity. It is assumed that a rock with high textural maturity has traveled a longer distance, as high maturity corresponds to more processes acting on the sediment and a longer time between erosion and deposition. Features to look for to determine maturity are grain size sorting, angularity/roundedness, and composition purity. Same-sized grains, round grains, and a single mineral type all indicate high textural maturity (this sediment forming this rock traveled far). A wide range of grain sizes, grains that are jagged, and a lot of different mineral grain types, all point to low textural maturity (this rock formed near it's source). And you can have combinations inbetween.
Coarse-grained phaneritic rocks have mineral grains that are large enough to be seen with the naked eye, giving them a rough texture. Fine-grained aphaneritic rocks have much smaller mineral grains that are not individually visible, resulting in a smooth or fine texture.
Deformational metamorphism is a type of metamorphism that occurs in response to tectonic stresses, like folding, faulting, or shearing. It can lead to the development of foliation or other textural features within the rocks. The changes are typically accompanied by recrystallization, but the mineralogical composition may remain relatively unchanged.
Soil texture is classified based on the relative proportions of sand, silt, and clay particles present in the soil. Soil texture is categorized into different classes such as sandy, loamy, or clayey, depending on the predominant particle size. The textural class of soil can influence properties such as water retention, drainage, and nutrient availability.
The texture of soil is determined by the proportion of sand, silt, and clay particles it contains. Sand particles are the largest, followed by silt, and then clay particles which are the smallest. The combination of these particle sizes influences properties such as drainage, nutrient retention, and aeration in the soil.
I think you might be referring to what is called textural maturity. It is assumed that a rock with high textural maturity has traveled a longer distance, as high maturity corresponds to more processes acting on the sediment and a longer time between erosion and deposition. Features to look for to determine maturity are grain size sorting, angularity/roundedness, and composition purity. Same-sized grains, round grains, and a single mineral type all indicate high textural maturity (this sediment forming this rock traveled far). A wide range of grain sizes, grains that are jagged, and a lot of different mineral grain types, all point to low textural maturity (this rock formed near it's source). And you can have combinations inbetween.
Artists use visual and real texture to make audiences recall textural experiences.
contrast
Modeling a flexible material, like clay, is a textural method of sculpture. Textural means to touch or form with the hands.
contrast
contrast
Textural criticism.
You can improve maturity by intelligence. Age also affects maturity of person.
•Geochemical, physical, and mineralogic (textural) changes that take place after burial of sediment -Not weathering -Not metamorphism/metasomatism
Movement and emotion are captured through textural variations.
brown bread provides a textural contrast to the soft prawn flesh.
Movement and emotion are captured through textural variations.