I don't know I'm looking for the same thing! Ugh!
Igneous rocks can be classified based on their texture and mineral composition. Texture is determined by the size of the mineral grains, with coarse-grained rocks forming from slow cooling and fine-grained rocks forming from rapid cooling. Mineral composition can also help differentiate igneous rocks, such as identifying the presence of minerals like quartz, feldspar, or olivine.
Rocks are classified into three main groups based on how they are formed: igneous rocks (formed from the cooling of molten rock), sedimentary rocks (formed from the accumulation and cementation of sediment particles), and metamorphic rocks (formed from the alteration of existing rocks under high heat and pressure). Each group has various subcategories based on specific characteristics and composition.
igneous rocks are made of lava that cools and hardens and metamorphic rocks are madeby heat and pressure.
Calloused rock, or Subtraceaneal rock. Also, Ephyloceaeoulical-Pharchylogenic Carboniferincean Postulate Aggrevations is a fancy way of saying it.
Color and texture is one way to classify igneous rocks. Another way to do this is modal classification and normative classification.
They are different because lava is when it hits earth's atmosphere; magma turns to lava. Magma is when its inside the volcano. They are different because of the color: darker/blacker and magma rocks are way hotter. Lava rocks are colder and fragile.
Rocks are mixtures and so do not have chemical formulas. Igneous rocks vary in composition, so there is no way of giving a formula.
because it is made by heat and intence crushing and dimonds and marble are both made this way.
The way in which they were formed.
because the way there formed is how there different
Rocks in the rock cycle are classified into three main types: igneous, sedimentary, and metamorphic. Igneous rocks are formed from cooling magma or lava, sedimentary rocks are formed from compressed sediments, and metamorphic rocks are formed from existing rocks that undergo heat and pressure changes. These three types of rocks interconnect and transform into one another through various geological processes in the rock cycle.
Earth materials can be classified based on their origin (igneous, sedimentary, metamorphic), composition (silicate minerals, carbonates, etc.), texture (grain size, shape), or physical properties (hardness, cleavage, color). Geologists use these characteristics to differentiate and categorize rocks and minerals found on Earth.