* Vesicular rock texture is generally displayed in extrusive igneous rocks which contain many vesicles of trapped air, such as pumice or scoria.
* Igneous rocks containing holes which were produced as gases escaped from the upper part of lava flow.
rocks are idenified by texture
Phaneritic is the texture of igneous rocks. These types of rocks crystallized slowly.
Usually have a rougher texture
Crystalline texture.
The relationship between an igneous rock's texture and where it was formed is that the texture depends on whether or not the rock is an extrusive rock or an intrusive rock. Those two different types of classifications for rocks tell you what the texture will be. For example, Intrusive rocks have a coarse-grained texture like granite and extrusive rocks have a fine-grained texture like basalt.
what is the texture of all inorganic land derived sedimentary rocks
Obsidian
The relationship between an igneous rock's texture and where it was formed is that the texture depends on whether or not the rock is an extrusive rock or an intrusive rock. Those two different types of classifications for rocks tell you what the texture will be. For example, Intrusive rocks have a coarse-grained texture like granite and extrusive rocks have a fine-grained texture like basalt.
Texture in rocks is not the same as color or shape. Texture refers to the size, shape, and arrangement of mineral grains or crystals within a rock, while color refers to the outward appearance of the rock. Similarly, shape in rocks refers to their physical form or structure, and not the internal arrangement of mineral grains which defines texture.
hard
The texture of rocks differs based on their formation processes and mineral composition. Igneous rocks typically have a crystalline texture, with interlocking mineral grains formed from cooling magma or lava. Sedimentary rocks often exhibit a layered or granular texture due to the accumulation and compaction of sediments. Metamorphic rocks may display a foliated or non-foliated texture, resulting from the alteration of existing rocks under heat and pressure, leading to the alignment of minerals or a more homogenous appearance.
Non-foliated Texture!