These are some characteristics which are used to help identify rocks: fracture, color, hardness, tenacity, texture, strata, banding, color, resistance to acids, and weight.
Lack of banding
grayish i think it just looks like rock
olivine, pyroxene, and calcium-rich plagioclase
No, shale rocks are not typically attracted to a magnet because they are composed primarily of clay minerals and other non-magnetic materials. Magnetism is generally not a characteristic of shale rocks.
A characteristic of all non-foliated metamorphic rocks is that they lack a layered or banded appearance, which distinguishes them from foliated metamorphic rocks. Instead, non-foliated rocks typically have a more uniform texture and are composed of interlocking mineral grains. Common examples include marble, formed from limestone, and quartzite, formed from sandstone. These rocks are often formed under conditions of high temperature and pressure but without significant differential stress.
Foliation is a characteristic of some metamorphic rocks.
rocky
Lack of banding
The mineral constituents of rocks are the major source of their color.
They can give you clues to how, when and where the rocks formed. :D
grayish i think it just looks like rock
Bills,lopoliths,batholiths,dyes,patholiths those r the characteristic of intrusive land form
No. Cell walls are a characteristic of some living things. Rocks do not live and do not have cells. Therefore they do not have cell walls.
The Characteristics are hard,soft,smooth,rough,large,small,etc.
Foliation, or the alignment of mineral grains in a preferred direction, tends to increase as rocks experience metamorphism. This results in a layered appearance in metamorphic rocks, such as schist and gneiss.
Large scale folding of rocks during mountain building is characteristic of compressional tectonic forces, such as in convergent plate boundaries where two tectonic plates collide. The folding of rocks results from the deformation caused by the compressional forces, leading to the formation of mountain ranges and fold structures.
olivine, pyroxene, and calcium-rich plagioclase