Geology is the study of the nonliving things that the Earth is made of. Geology is the study of rocks in the Earth's crust. People who study geology are called geologists. Some geologists study minerals and the useful substances the rocks contain (such as natural gas and oil). Geologists also study the history of the Earth.
Geology is divided into special subjects that study one part of geology. Some of these subjects are:
- Geomorphology – the study of the shape (morphology) of the surface of the Earth.
- Historical geology – the history of the events that shaped the Earth over the last 4.5 million years.
- Hydrogeology – the study of water under the surface of the Earth
- Palaeontology – the study of fossils
- Petrology – the study of rocks how they form and where they are from.
- Mineralogy – the study of minerals
- Sedimentology – the study of sediments
- Stratigraphy – the study of layered sedimentary rocks and how they were deposited.
- Structural geology– the study of folds and faults and how mountains are formed by uplift. See Earth science
- Volcanology – the study of volcanoes on land or under the ocean
- Seismology – the study of earthquakes and strong ground-motion.
- Engineering geology -the study of geologic hazards (such as landslides and earthquakes) applied to civil engineering.
- Petroleum geology- the study of petroleum deposits in sedimentary rocks.
Types of rock[change | change source]
Rocks can be found in all sorts of shapes and colours. Some are very hard and some are soft. Some rocks are very common, while others are rare. However, all the different rocks belong to three categories or types, igneous, sedimentary and metamorphic.
Igneous rock[change | change source]
Igneous rock is rock that has been made by volcanic action. Igneous rock is made when the lava (melted rock on the surface of the Earth) or magma (melted rock below the surface of the Earth) cools down and becomes hard.
Sedimentary rock[change | change source]
Sedimentary rock is rock that has been made from sediment. Sediment is all solid pieces of stuff that are moved by the wind, water, or glaciers. Sediment can be made from clay, sand, gravel and the bodies and shells of animals. The sediment gets dropped in a layer at the bottom of a river or sea. As the sediment piles up, the lowers layers get squashed together. Slowly they set hard into rock. Some sedimentary rocks are made of just one type of sediment, all about the same size, such as sand. Other sedimentary rocks will have large and small lumps, and pieces made of different types of rock. Well-known sedimentary rocks are sandstone and limestone.
Metamorphic rock[change | change source]
Metamorphic rock is rock that has been changed. The word "metamorphosis" means "change". Sometimes an igneous, or a sedimentary rock can be heated, or squashed under the ground, so that it changes. Metamorphic rock is often harder than the rock that it was before it changed. One well-known metamorphic rock is marble which is valued for its different colours, and because it can be carved and polished. Slate is a metamorphic rock that is a useful building material.
Faults[change | change source]
All three kinds of rock can be changed by being heated and squeezed by forces in the earth. When this happens, faults (cracks) may appear in the rock. Geologists can learn a lot about the history of the rock by studying the patterns of the fault lines. Earthquakes are caused when a fault breaks suddenly.
Soil[change | change source]
Soil is the stuff on the ground made of lots of particles (or tiny pieces). The particles of soil come from rocks that have broken down, and from rotting leaves and animals bodies. Soil covers a lot of the surface of the Earth. Plants of all sorts grow in soil.
Principles of Stratigraphy[change | change source]
Geologists use some simple ideas which help them to understand the rocks they are studying. The following ideas were worked out in the early days of stratigraphy by people like Nicolaus Steno, James Hutton and William Smith:
- Understanding the past: Geologist James Hutton said "The present is the key to the past". He meant that the sort of changes that are happening to the Earth's surface now are the same sorts of things that happened in the past. Geologists can understand things that happened millions of years ago, by looking at the changes which are happening today.
- Horizontal strata: The layers in a sedimentary rock must have been horizontal (flat) when they were deposited (laid down).
- The age of the strata: Layers at the bottom must be older than layers at the top, unless all the rocks have been turned over.
- In sedimentary rocks that are made of sand or gravel, the sand or gravel must have come from an older rock.
- The age of faults: If there is a crack or fault in a rock, then the fault is younger than the rock. Rocks are in strata (lots of layers). A geologist can see if the faults go through all the layer, or only some. This helps to tell the age of the rocks.
- The age of a rock which cuts through other rocks: If an igneous rock cuts across sedimentary layers, it must be younger than the sedimentary rock.
- The relative age of fossils: A fossil in one rock type must be about the same age as the same type of fossil in the same type of rock in a different place. Likewise, a fossil in a rock layer below must be earlier than one in a higher layer.
Gallery[change | change source]
A fault cutting through older sedimentary rocks
A conglomerate: sedimentary rock made from white pieces of older rock, broken up and mixed with red sand at the bottom of a river.
The geologist, David Johnston, on the side of Mount St. Helens.
Geologists look at some samples of rock, to find minerals for mining.
Related pages[change | change source]
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