Unit 4: Minerals and rocks                                                       1   2   3   4

 

 

3.3. Sedimentary rocks

 

a) Types of sedimentary rocks

 

     Sedimentary rocks are classified into three groups: detrital,

     chemical and organic.

 

       - Detrital rocks are made up of fragments of other rocks

         that are stuck together.

 

       - Chemical sedimentary rocks are made of mineral crystals

          from oceans, lakes and groundwater that have dissolved in water.

 

       - Organic sedimentary rocks are made of plant and animal

         remains which have been transformed into minerals.

 

b) Formation of sedimentary rocks

 

     It begins with the accumulation and consolidation of sediment

     or of rock fragments.

  

     Rocks are fragmented by:

 

         - Weathering.

           Rocks at the surface of the Earth are broken up

           by the action of atmospheric phenomena (changes in

           temperature, rain, etc), or by the activities of plants and

           animals.

        

        - Erosion.

           These broken fragments of rocks are swept away

           by running water, glaciers, waves or wind.

 

    The deposited sediments are transformed into compact, cohesive   

    rocks by two processes:

        - Compaction. The weight of successive layers of sediment

          compacts the sediments. This pressure reduces the spaces

          between the fragments and squeezes out the water.

          As a resultsalt crystals are formed.

 

       - Cementation. The rock fragments are stuck together

          with the salt crystal which formed when the water was

          eliminated 

     Each layer of sediments is transformed into a layer of sedimentary 

     rock, called a stratum.  

 

    Organic sedimentary rocks are formed because the rests of vegetation

    and microscopic marine animals and plants was covered

    quickly by sediments, avoiding the putrefaction. In this environment,

    of high pressure and temperature and without air, some kind of

    bacteria changes the organic matter into coal or oil.

 

c) Fossils

 

     Sedimentary rocks sometimes

     contain remains of living things

     that lived millions of years ago.

    

     These remains are called fossils.

     Fossils become part of the rocks,

     during the processes of compaction

     and cementation of sediments.

 

     Fossils provide invaluable

     information about the history

     of life on Earth.

 

READING ACTIVITIES

 

After reading the text, copy and answer the following questions into your notebook:

Remember: you must make complete sentences.

 

3.7. Name some examples of:

       a. Detrital sedimentary rocks

       b. Chemical sedimentary rocks

       c. Organic sedimentary rocks

 

3.8. Define:

       a. Compaction

       b. Fossil

       c. Stratum

 

   

1   2   3   4


   

  Wordreference

  (Diccionario Ing-Esp)

  

  Wordreference games 

  (Juegos de vocabulario)

  

  Merrian Webster

  (Visual dictionary)

 

  Infovisual

  (Visual dictionary)

  

  Eduplace

  (Glosario de C. Naturales)

 

  Linguaframe 1ESO

  (Science audio-glossary)

 

  Linguaframe 2ESO 

  (Science audio-glossary)

  

  Oodcast

  (Pronunciación)

  

  Glossopedia

  (Enciclopedia de C. Naturales)

 

  Web elements 

  (Tabla periódica)

 

 

  Eva Mª

  López Rodríguez

 

  Departamento

  Biología y Geología

 

  IES " J. S. Elcano"

  Sanlúcar de Barrameda