A Level Geology Eduqas

This subject is broken down into 31 topics in 8 modules:

  1. Fundamentals of Geology 5 topics
  2. Rocks and Minerals 4 topics
  3. Coastal Processes and Features 3 topics
  4. Tectonic Processes and Hazards 4 topics
  5. Geological Resources and the Environmental Impact 5 topics
  6. Geotechnics 3 topics
  7. Glaciation 3 topics
  8. Geological Evolution of the British Isles 4 topics
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  • 8
    modules
  • 31
    topics
  • 12,396
    words of revision content
  • 1+
    hours of audio lessons

This page was last modified on 28 September 2024.

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Geology

Fundamentals of Geology

Rocks and minerals

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Rocks and minerals

Rocks and Minerals Overview

  • Rocks are comprised of minerals, which are naturally occurring, inorganic solids that have a specific chemical formula and defined crystal structure.
  • Minerals have physical properties that can be used for identification, including: colour, lustre, streak, hardness, cleavage, fracture and crystal shape.
  • Rocks are classifiable as igneous, sedimentary, or metamorphic, based largely upon their formation processes.
  • The rock cycle illustrates the transitions between these three rock types: igneous rocks convert to sedimentary rocks through weathering and erosion, which can then become metamorphic rocks through intense heat and pressure. This cycle can be repeated.

Igneous Rocks

  • Igneous rocks are formed from the solidification of magma or lava.
  • They may be intrusive (formed within the earth’s surface, such as granite) or extrusive (formed on the earth’s surface, like basalt).
  • These rocks can be distinguished by their texture, classified as coarse-grained, fine-grained, or glassy.
  • Common igneous rocks include granite, basalt, and pumice.

Sedimentary Rocks

  • Sedimentary rocks are formed through the accumulation and compaction of sediments.
  • They are classified into clastic, chemical, and organic, depending on the type of sedimentation process.
  • Features like stratification, fossils, and ripple marks can typically be found in sedimentary rocks.
  • Well-known examples are limestone, sandstone, and shale.

Metamorphic Rocks

  • Metamorphic rocks originate from existing rocks, which are transformed by high temperature or pressure but do not melt.
  • They are categorized as contact (caused by heat) or regional (due to pressure) metamorphic rocks.
  • Telling features can include foliation, a layering due to pressure.
  • Common examples include slate, marble, and gneiss.

Significance of Rocks and Minerals

  • Rocks and minerals are significant for understanding the Earth's history, exploring for natural resources, and predicting the potential for natural hazards.
  • Studying rock strata can provide information about past climates and events, as well as chronological data for geologic history.
  • The exploration for oil, natural gas, and minerals relies on understanding the geological principles related to rocks and minerals.
  • Measurement of rock and mineral properties can indicate the likelihood of earth activities such as earthquakes and volcanic eruptions.

Course material for Geology, module Fundamentals of Geology, topic Rocks and minerals

Geology

Geological Resources and the Environmental Impact

Fossils and paleontology

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Fossils and paleontology

Understanding Fossils and Paleontology

  • Fossils are the preserved remains or traces of animals, plants, and other organisms from the past.
  • Fossils can preserve hard parts like bones and shells, as well as soft tissues in exceptional conditions.
  • The fossil record is a term used to describe the total number of fossils discovered and the information they provide about the history of life on Earth.
  • The study of fossils is known as paleontology.
  • Fossil record is incomplete due to the selective preservation of organisms and lack of discovery of many fossils.
  • The process of fossilisation includes permineralisation, replacement, cast and mould formation, carbonisation and imprintation.

Types of Fossils

  • Body fossils: These include parts of organisms, such as bones, teeth, and shells.
  • Trace fossils: These include signs of biological activity, such as footprints, burrows and coprolites.
  • Chemical fossils: Also called chemofossils, these include biochemical and chemical residues.

Dating Fossils

  • Relative dating and absolute/numerical dating are the two methods for dating fossils and rocks.
  • Relative dating establishes a sequence of events but does not provide exact dates.
  • Absolute dating provides a numerical age using techniques like radiometric dating.
  • Radioactive decay, half-life, and radiocarbon dating are key concepts in understanding absolute dating.

Interpreting Fossils

  • Fossils provide information about the past climate and environment, known as paleoenvironment.
  • Fossils demonstrate evidence of evolution, showing how species have changed over time.
  • Index fossils are useful for dating and correlating the age of rocks, being known to have lived over a short time range but have a wide geographical distribution.
  • Fossil assemblages can help determine the relative age of rocks.
  • Paleontologists use biostratigraphy, the study of the vertical distribution of fossils within rocks, to detect changes over geological time.

Fossils and Geological Resources

  • Fossil fuels (coal, oil, natural gas) are biogenic substances formed from the remains of dead plants and animals over millions of years.
  • The formation of fossil fuels involves processes of compaction, heat and pressure, and requires specific environmental conditions.
  • Coal formation follows a sequence from peat, lignite, sub-bituminous, bituminous to anthracite.
  • Oil and natural gas are typically found in sedimentary rocks and are associated with source rocks, reservoir rocks, and trap structures.
  • Fossil fuels exploration involves methods like seismic surveying, drilling, and geological mapping.
  • Overreliance on fossil fuels has environmental impacts, including air pollution and climate change.

Preservation and Conservation

  • Fossils are non-renewable resources that need to be proteced for future research and education.
  • Fossil sites may be designated as protected areas, or Sites of Special Scientific Interest (SSSIs), to avoid damage and unauthorized collection.
  • There is a legal and ethical responsibility for collection and trade of fossils, with some requiring permits or restricted under law.

Course material for Geology, module Geological Resources and the Environmental Impact, topic Fossils and paleontology

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