Geological Properties Of The Three Types Of Rocks

 

The three types of rocks

Igneous — they form from the cooling of magma deep inside the earth. They often have large crystals (you can see them with the naked eye).

Metamorphic — they are formed through the change (metamorphosis) of igneous and sedimentary rocks. They can form both underground and at the surface.

Sedimentary — they are formed through the solidification of sediment. They can be formed from organic remains (such as limestone), or from the cementing of other rocks.
Now the long story, which is much more interesting, is this:

 

Igneous Rocks

Magma is the heart of any igneous rock. Magma is composed of a mixture of molten or semi-molten rock, along with gases and other volatile elements. As you go deeper underground, the temperature rises; go further and you’ll eventually reach the Earth’s mantle — a huge layer of solid rock surrounding the Earth’s core (which, in geologic time, behaves as a viscous liquid).

As you probably know, when magma cools, it turns into rock; if it cools while still underground at high temperatures (but at temperatures still lower than that of the magma), the cooling process will be slow, giving crystals time to develop. That’s why you see rocks such as granite with big crystals — the magma had time to cool off. The crystals are also differentiated, as you can see below.

However, if the magma erupts or is cooled rapidly, you instead get a volcanic rock –– not really igneous, but also originating from lava. The classical example here is basalt, which can have many small crystals or very few large ones. Volcanic rocks are also called extrusive igneous rocks, as opposed to intrusive igneous rocks. Some volcanic rocks (like obsidian) don’t have any crystals at all.

Not all magma is made equally: different magmas can have different chemical compositions, different quantities of gases and different temperature — and different types of magma make different types of rocks. That’s why you get incredible variety. There are over 700 hundred types of igneous rocks, and they are generally the hardest and heaviest of all rocks. However, volcanic rocks can be incredibly lightweight –– pumice, for example, can even float, and was called by ancient sailors “the foam of the sea”. Pumice is created when a volcano violently erupts, creating pockets of air in the rock. 

 

Spiritual Reflection:

Igneous rocks embody creation, transformation, and the raw power of beginnings. They symbolize grounding, purification, and the courage to forge new paths from the fires of change, much like crystals such as Obsidian or Andesine that emerge from volcanic origins.

 

The Most Common igneous rocks are:

andesite
basalt
dacite
dolerite (also called diabase)
gabbro
diorite
peridotite
nepheline
obsidian
scoria
tuff
volcanic bomb

 

Metamorphic Rocks

Here, the name says it all. These are rocks that underwent a metamorphosis; they changed. They were either sedimentary or igneous (or even metamorphic), and they changed so much, that they are fundamentally different from the initial rock.

There are two types of metamorphism (change) that can cause this:

contact metamorphism (or thermal metamorphism) — rocks are so close to magma that they start to partially melt and change their properties. You can have recrystallization, fusing between crystals and a lot of other chemical reactions. Temperature is the main driver here.

regional metamorphism (or dynamic metamorphism) — this typically happens when rocks are deep underground and they are subjected to massive pressure — so much so that they often become elongated, destroying the original features. Pressure (often times with temperature) is the main driver here.

Metamorphic rocks can have crystals and minerals from the initial rocks as well as new minerals resulting from the metamorphosis process. However, some minerals are clear indicators of a metamorphic process. Among these, the most usual ones are garnet, chlorite, and kyanite.

Equally as significant are changes in the chemical environment that result in two metamorphic processes: mechanical dislocation (the rock or some minerals are physically altered) and chemical recrystallization (when the temperature and pressure changes, some crystals aren’t stable, causing them to change into other crystals).

They can be divided into many categories, but they are typically split into:

Foliated metamorphic rocks — pressure squeezes or elongates the crystals, resulting in a clear preferential alignment.

Non-foliated metamorphic rocks — the crystals have no preferential alignment. Some rocks, such as marble (the metamorphized version of limestone), are made of minerals that simply don’t elongate, no matter how much stress you apply.

Metamorphic rocks can form in different conditions, in different temperatures (up to 200 °C) and pressures (up to 1500 bars). By being buried deep enough for a long enough time, a rock will become metamorphic. They can form from tectonic processes such as continental collisions, which cause horizontal pressure, friction and distortion; they can also form when the rock is heated up by the intrusion of magma from the Earth’s interior.

 

Spiritual Reflection:

Metamorphic rocks symbolize transformation, resilience, and spiritual evolution. Just as they are reborn under pressure, they remind us that personal and spiritual growth often arises from life’s most intense experiences. Crystals such as Labradorite, Garnet in Astrophyllite, and Tremolite echo this profound metamorphic energy.

 

The most common metamorphic rocks are:

amphibolite
schist (blueschist, greenschist, micaschist, etc)
eclogite
gneiss
hornfels
marble
migmatite
phyllite
quartzite
serpentinite
slate

 

Sedimentary Rocks

Sedimentary rocks are named as such because they were once sediment. Sediment is a naturally occurring material that is broken down by the processes of weathering and erosion and is subsequently naturally transported (or not). Sedimentary rocks form through the deposition of material at the Earth’s surface and within bodies of water.

Sedimentary rocks are quite difficult to classify, as they have several different defining qualities (the chemical make-up, the sedimentation process, organic/inorganic material), but the most common classification is the following:

clastic sedimentary rocks — small rock fragments (many silicates) that were transported and deposited by fluids (water, bed flows). These rocks are further classified by the size and composition of the clastic crystals included in the sedimentary rocks (most often quartz, feldspar, mica and clay).

conglomerates (and breccias) — conglomerates are predominantly composed of rounded gravel, while breccias are composed of angular (sharper) gravel.

sandstones — as the name says, it’s a rock made from many-sand-sized minerals and rock grains. The most dominant mineral in sandstone is quartz because it is the most common mineral in the Earth’s surface crust.

mudrocks — again, the name says it all — they’re rocks made from solidified mud. They typically contain very fine particles and are transported as suspended particles by turbulent flow in water or air, depositing once the flow settles.

Geological Properties Of The Three Types Of Rocks

biochemical rocks — you’ll probably be surprised to find out that most limestone on the face of the Earth comes from biological sources. In other words, most limestone you see today comes from the skeletons of organisms such as corals, mollusks, and foraminifera. Coal is another example of biochemical rock.

chemical rocks — these rocks include gypsum and salt (halite) and are formed mostly through water evaporation.

There are also other types of specific sedimentary rocks — for example, the ones formed in hot springs. Most of the solid surface of our planet (roughly 70%) is represented by sedimentary rocks, but if you go deep enough beneath the Earth’s surface, there are plenty of igneous and metamorphic rocks to be found.

 

Spiritual Reflection:

Sedimentary rocks carry the vibration of memory and patience. They remind us that transformation takes time — layer by layer, experience by experience. Stones such as Turritella Agate and Jasper embody this energy, grounding us in the wisdom of the Earth’s long cycles.

 

Some common sedimentary rocks are:

argillite
breccia
chalk
chert
claystone
coal
conglomerate
dolomite
limestone
gypsum
greywacke
mudstone
shale
siltstone
turbidite

 

At Crystals by Rob

At Crystals by Rob, we celebrate the Earth’s natural artistry through its rocks and minerals. Every crystal begins as part of this grand geological cycle — from fiery creation to layered history and transformative rebirth. Our mission is to honor these origins, blending geological knowledge with spiritual insight. Each piece in our collection carries the story of the planet’s journey, inviting you to connect with the elemental forces that shape both the Earth and the spirit.