New crystal nucleation rates, which is how enough chemical components can come together without dissolving, is another factor affecting the texture. The rate of crystal growth is another factor, and that's how quickly new constituents come to the surface of the growing crystal. Other factors include the diffusion rate, which is how atoms and molecules move through the liquid. Includes line/area/bar/stacked charts, pie/donut charts, scatter plots, swimlanes, flamechart, sunburst, sankey flow graphs, data tables, etc. What determines igneous rock texture? It all comes down to the rate at which the rock cools. Configurable Chart Collection: A variety of visualizations with a declarative and extensible API. Each kind of texture has a variety of different characteristics that make them unique. There are nine main types of igneous rock textures: Phaneritic, vesicular, aphanitic, porphyritic, poikilitic, glassy, pyroclastic, equigranular, and spinifex. Larger scale features, such as fractures and layering, are considered rock structures in comparison. This includes the size and quality and interrelations of its grains and the fabric they form.
The texture of a rock refers to the details of its visible character.
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