The rock would have visible mineral crystals--a phaneritic texture.
Hardness usually is used to describe the difficulty of separating the molecules of a material or substance. The texture is simply how the material or substance feels.
Actual texture is texture that you can feel, whereas visual or implied texture is when something looks like it has a texture it does not. For instance, the actual texture of a painting may be smooth, but the visual/implied texture may be rough and bumpy.
the tree bark has a different texture and style and the cottonwood has softer bark. xxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxxx
Real texture physically exists on the art object- consider rust on a metal statue, or thickly-applied paint on an oil painting. Visual texture is the aesthetic representation of real texture- consider a photograph of rust. It shows the texture, but the photograph itself is smooth. Likewise, a smooth painting depicting rust.
The display a phaneritic texture.
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.
Texture
The texture of igneous rocks with large crystals that form from slow cooling is called phaneritic. This texture indicates that the minerals had enough time to grow large enough to be visible to the naked eye. Examples of rocks with phaneritic texture include granite and diorite.
Phaneritic is the texture of igneous rocks. These types of rocks crystallized slowly.
phaneritic
Different clastic sediments have different textures based on the size, shape, and sorting of the grains they are composed of. The composition of a clastic sedimentary rock will vary depending on the mineralogy of the grains present in the rock. Factors such as the source rock, transportation distance, and depositional environment can all contribute to the differences in texture and composition between clastic sedimentary rocks.
Coarse-grained phaneritic rocks have large, visible crystals that formed slowly beneath the Earth's surface, giving them a rough texture. In contrast, fine-grained aphanitic rocks have tiny crystals that formed quickly at or near the Earth's surface, resulting in a smooth texture without visible crystals.
Granite rock is not porphyritic. It is phaneritic because it has a coarse-grained texture.
Large size crystals that are known as phaneritic are typically found in intrusive igneous rocks. These rocks cool slowly beneath the Earth's surface, allowing the crystals time to grow to visible sizes. Phaneritic textures are characterized by crystals that are easily visible to the naked eye.
Coarse grained.
And their texture, which can be aphanitic, phaneritic, glassy, or porphyritic. mineral composition and crystal texture