There is more than one way to answer your question, and if you are given a hand sample (like a chunk of rock) sometimes its hard to tell!
Here are some hints that can lead you figure out if a rock is sedimentary, igneous, or metamorphic
If a rock is sedimentary:
it will be composed of grains, or clasts, from other rocks. Sandstones, for example, will be made up of primarily sand grains. Siltstones, clay stones, or grainstones, will have smaller grains that you might not be able to see with the naked eye! Often sedimentary rocks are porous, which means they have little holes that can hold fluids, like water. can you rub the rock and feel grains coming off in your hand? you might have a sedimentary rock. Do you see fossils in the rock? Its most likely sedimentary.
If a rock is igneous;
you need to know what minerals may indicate igneous origin. if the rock is a plutonic igneous rock, it will have large grains, and you will probably see feldspars, biotite, pyroxene, and amphibole. Volcanic rocks will be finer grained, so you need to look for structures and textures that would indicate a volcanic origin. If the rock is massive, i.e, no orientation of grains, and no structures are present, you may have a volcanic igneous rock. If your rock is glassy, like obsidian, you may have a volcanic igneous rock. if your rock has holes in it, like pumice, you may have a volcanic igneous rock
If the rock is metamorphic;
again, you need to look for certain minerals and structures that could point you to this conclusion. If you see chlorite, a harder green mica, you probably have a metamorphic rock. If the rock looks like a sandstone but isn't porous, you have quartzite, a metamorphosed sand stone. If you see foliation (like paper thin layers, perhaps not linear), or deformation structures (like stretched or deformed crystals) there is a good chance you have a metamorphic rock.
While some areas may have more of one type of rock than another area, try not to generalize the area until you know what may be causing these types of rocks.
Geological principles tell us that inclusions are pieces of older rock that are included within a younger rock formation. Inclusions are helpful in determining the relative ages of rock layers, as the rock containing the inclusion must be younger than the inclusion itself. Additionally, the types of inclusions present can provide information about the environment in which the rocks formed.
You can tell if a rock is weathering by observing physical changes such as cracking, chipping, or crumbling, as well as changes in color or texture. Weathering can also be indicated by the presence of weathering agents like water, wind, or plants acting on the rock surface.
A rock within a rock, also known as an inclusion, forms when a pre-existing rock gets trapped within another rock during the formation process. This can happen through processes like sedimentation or volcanic activity. Over time, the outer rock solidifies around the inner rock, creating a distinct feature in the final rock formation.
A geologist could tell you what kind of rock that is. I am studying to become a geologist.
Undisturbed rock layers can provide valuable information about Earth's history. By studying the order and sequence of rock layers, scientists can determine the relative ages of the rocks and understand the past environments, climate, and geological events that shaped the Earth. Fossils found in these undisturbed layers can also provide insights into past life forms and evolution.
Bauxite is a sedimentary rock that is formed through the weathering and precipitation of aluminum-rich minerals such as gibbsite, boehmite, and diaspore. These minerals are derived from the weathering of aluminum-rich rocks like granite and basalt.
There are lots of different types of rocks in the world.
You could tell an older rock from a younger rock by looking at it because the older rock isochron would have a steeper slope.
a rock is never alive
A rock is made of different minerals.
A metamorphic rock will display foliation or bands around the rock.
Bauxite is primarily classified as a sedimentary rock. It forms through the weathering and leaching of aluminum-rich rocks in tropical and subtropical environments, typically through the process of laterization. While it can contain minerals that are derived from igneous sources, its formation process does not involve igneous or metamorphic processes.
sedimentary rock is a multiple of layers
if you take a magnet and put it on two rocks then the meteor rock will attract and the other rock will stay
It is not so you cannot ever tell.
Well The Igneous Rock: When it Forms Underground the Pressure combines with Large crystals :)
You tell me