Earth Geology

The world of TerraFirmaGreg is divided into large continents - landmasses many kilometers wide and seperated by oceans. In these, you may find mountain ranges, rivers, and many other formations. Here you will learn about the geology of Earth and how rock layers are determined.

• Rock Layers
• Metamorphism
• Ocean Floors
• Uplift Regions
• Rock Devisions
• Sedimentary
• Metamorphic
• Igneous Extrusive
• Igneous Intrusive
• Rock Classifiers
• Sedimentary-Carbonate
• Sedimentary-Clastic
• Sedimentary-Organic
• Igneous-Felsic
• Igneous-Intermediate
• Igneous-Mafic
• Igneous-ultramafic

Camadas de Rocha

The world is divided up into different types of Rock. Rock regions can be over a kilometer across, and there will usually be two or three different rock layers under your feet at all times. As different ores are found in different rock types, locating specific rock types can be very important for finding resources such as Ores, which will often only appear in certain rock types.

A camada superior de rocha em um continente será ou ígnea extrusiva ou sedimentar. Abaixo das rochas sedimentares, provavelmente haverá formas metamorfoseadas da rocha acima.

Por exemplo, Mármore (uma rocha metamórfica) provavelmente será encontrada abaixo de Calcário ou Giz. Rochas metamórficas de alto grau são encontradas profundamente abaixo de outras rochas metamórficas ou ígneas.

Metamorphism

• Ardósia se forma sob Folhelho, Argilito e Conglomerado.
• Mármore se forma sob Calcário, Dolomita e Giz.
• Quartzito se forma sob Cherte.
• Filito se forma sob Ardósia.
• Folhelho e Gnaisse se formam sob Filito, ou outras rochas ígneas intrusivas.

Fundo dos Oceanos

O fundo do oceano é composto por rochas ígneas extrusivas - rochas formadas por magma que resfria rapidamente. Abaixo da rocha ígnea extrusiva, provavelmente haverá uma rocha ígnea intrusiva do mesmo grau.

Por exemplo, sob o Basalto (uma rocha ígnea extrusiva, máfica), provavelmente haverá Gabro (uma rocha ígnea intrusiva, máfica).

Uplift Regions

Finally, in mountainous regions you might also see uplift, where a metamorphic or igneous intrusive rock is found on the surface. Uplift rocks can be found above other continental sedimentary or higher-grade metamorphic rocks.

In addition, Dikes↪ - small vertical slices of igneous intrusive rock - may appear scattered around the world.

Rock Devisions

Rocks in TFG are typically classified among four devisions: Sedimentary, Metamorphic, Igneous Extrusive, and Igneous Intrusive. These categories determine where the rock can spawn, and also what ores may spawn in this rock.

Sedimentary↪ rocks are formed by the accumulation or deposition of mineral or organic particles. They are typically found on the top layers of rock in continental areas.

Metamorphic↪ rocks are created by a process called metamorphism. They can be found underneath corresponding sedimentary or igneous rock, or in uplift areas.

Igneous Extrusive↪ rocks are formed from magma cooling on the Earth's surface. They can be found on the top layer of rock in continental areas, or on the floor of oceans.

Igneous Intrusive↪ rocks are formed from magma which cooled under the Earth's crust. They can be found deep underground, or rarely in dikes or uplift areas.

Rock Classifiers

On top of Rock Devisions, rocks are further categorized by their chemical compositions.

Sedimentary-Carbonate↪ rocks are composed primarily of carbonate minerals like calcite.

Sedimentary-Clastic↪ rocks are composed of fragmants (clasts) of pre-existing minerals or rocks.

Sedimentary-Organic↪ rocks are formed from the breakdown or fossilization of organic matter like shells or bacteria.

Igneous-Felsic↪ rocks contain a rich presence of elements that form feldspar and quartz. Generally a rock must contain more than 75% of felsic minerals to be classified as Felsic.

Igneous-Intermediate↪ rocks contain 51.5 - 63.0 wt% SiO₂, putting them in between Felsic and Mafic compositions.

Igneous-Mafic↪ rocks contain a rich presence of magnesium and iron minerals.

Igneous-Ultramafic↪ rocks contain a very low concentration of silica.