Lesson 9 geological chronology. Geological chronology

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Geography teacher Beznogova O.N. Municipal educational institution "Privalenskaya secondary school" of the Omsk region exit Geological chronology Geological chronology Geochronological table Geochronological table Geological map Geological map resources




Geological chronology (geochronology) Relative age Relative age Relative age Relative age Absolute age Absolute age Absolute age Absolute age Determined by the occurrence of rocks not disturbed in a later period and fossil remains - fossils. Determined by the ratio of the content of a radioactive element in a rock and its decay products. Other sciences that study the earth's crust Other sciences that study the earth's crust Other sciences that study the earth's crust Other sciences that study the earth's crust exit back The rocks that make up the earth's crust were formed at different times. The branch of geology that studies the age, duration, and sequence of formation of rocks.


Historical geology Geotectonics Paleontology Mineralogy Petrography What does it study? Studies the patterns of the structure of the earth's crust over geological time. The study of the structure of the earth's crust and the formation of tectonic structures. The science of extinct organisms studied from fossils, preserved hard skeletons, etc. The science that studies minerals. The science that studies rocks. Geochronology - studies the age, duration, sequence of formation of rocks. Branches Geology, studies the structure and history of the development of the Earth. exit back


Geochronological table Era, group The entire geological history of the Earth is divided into eras - large periods of time in the history of the Earth. (AR, PR, Pz, Mz, Kz). The entire geological history of the Earth is divided into eras - large periods of time in the history of the Earth. (AR, PR, Pz, Mz, Kz). The period, the Era system is divided into periods (see the tip for how easier it is to remember them). Hint K Every O Excellent St Student D Must K Smoke P Cigarettes T You Yu Yura M Mal P Wait N A Little Four Years K Every O Excellent St Student D Must K Smoke P Cigarettes T You Yu Yura M Mal P Wait N A Little H Four Years Contains information about the successive change of eras and periods in the development of the Earth and their duration. Contains information about the successive change of eras and periods in the development of the Earth and their duration. Museum (Internet) exit back table


Geological map Conventional signs A geological map allows you to get an idea of ​​the distribution of rocks of different ages and origins. The territory of the southern part of the Omsk region is composed of sedimentary rocks of Neogene age. Example exit back


Slide 2 – drawing from the CD “Geography. Planet Earth" for 6th grade. JSC Publishing House Prosveshcheniye Screenshots of maps were taken from disk maps K and M hammer jpg outcrop 7dbf40b95f96/004.swfhttp://files.school-collection.edu.ru/dlrstore/aa16a505-4efc-4dad-ab71-7dbf40b95f96/004. swf tectonic map exhibits of the museum of paleontology exit back

"Verified"_________________

Short-term geography lesson plan 8.2.1.1.

Lesson No.

Class8

date

Lesson topic:

Geological chronology

Target:

Study the features of geological chronology

Educational educational tasks:

To develop knowledge about the absolute and relative ages of rocks. Reveal the structure of the geochronological table. Develop skills and abilities to work with a geochronological table. Develop analytical thinking and the ability to express your own opinion.

Instilling values

Values ​​based on the national idea “Mangilik El”:

Foster an active life position

Lesson type

Learning new material

Forms

Frontal, collective, group individual-isolated

Methods

Verbal, visual, reproductive

Modules

New approaches, RCM, ICT, ODO, ROiT, LU, VO

Equipment and

visual

benefits:

Physical map, tectonic map, geological map, geochronological table PC - presentation “Geological chronology”

Expected Result

All students will be able to name:

1. Stages of development of the Earth: planetary and geological.

2. Methods for determining the age of rocks.

3. Eras of Earth's development

Most students will be able to

Use a geochronological table.

Correlate eras-periods-duration

Some students will be able to

Talk about the patterns of geological processes, work with a geochronological table

Working with terms and concepts

Geology, tectonics, earth's crust, lithosphere, eras, periods, folding, plates and platforms, relief formation

Geographical objects:

Russian Platform, Turanian Plate, Gondwana, Laurasia

During the classes.

Lesson steps

Planned activities

Resources

Lesson starts 7-10 minutes

    Organizing time. Organization optimal conditions for educational activities. Checking student attendance.

    Activation of cognitive activity

    What is the name of the country we live in?

    What continent is Kazakhstan on?

    In what part of the Eurasian continent is Kazakhstan located?

    Which countries does Kazakhstan border with?

    What landforms predominate in Kazakhstan?

    In what part of Kazakhstan are the mountains located?

    Name the highest peak in Kazakhstan

    Name the lowest point in Kazakhstan

    What large plains do you know?

    What mountain ranges are there in Kazakhstan?

    Watch the video “history of the earth in 5 minutes”

    Statement of the problem situation:

- Is the appearance of the earth’s surface of our country, its nature, random?

-Have they always been like this?

-If not, how and why did they change?

-How did scientists prove that nature was constantly changing and developing?

We have to answer these questions. Be careful.

Reception "Pass" - ball

PC - video

Mid-lesson 20-25 min

1. Introduction “People guessed that the nature of the Earth was not always the way people see it when they encountered fossils, plants and animals that no longer exist, and shells. Gradually, the science of ancient life—paleontology—was formed. What are the names of scientists involved in this science?

For many years, scientists around the world have been studying the preserved remains of animals and plants found in strictly defined layers of rocks. This means that the development of nature is inextricably linked with geological development, so they must be considered in unity. Currently, scientists have reconstructed a picture of the Earth's past by creating a geochronological table.

Determining the age of rocks allows us to establish the relative and absolute time that has passed since some moment or event in the history of the Earth. If the occurrence of rocks is not disturbed, then each layer is younger than the one on which it lies. The topmost layer was formed later than all those lying below. The time during which each group of rocks accumulated is called an era. Era name reflects relative time

How is the absolute age of rocks determined?

Absolute age is the time elapsed since the rock was formed. It is determined by radioactive elements - for example, uranium. The rate of its decay is known and always remains unchanged (uranium decays into helium and lead, helium is seeded, lead remains) by the amount of lead the age of the rock is determined

Conclusion : Rocks are witnesses to the evolution of life

2. Working with a geochronological table pp. 34-35

Individual work turns into group work: students write down everything they know on this topic, or can extract from the table:

Which graphs stand out in it?

Read the names of the periods of each era from the oldest to the youngest.

What was the longest era in Earth's history?

Which periods were the longest?

Which period is the shortest?

What changes occurred in nature in each era?

What is the name of the era and period in which we live?

They exchange baskets, read and discuss.

3. Group work

1. group – Archean and Proterozoic era

Group 2 – Paleozoic era

Group 3 – Mesozoic era

Group 4 – Cenazoic era

Using atlas maps, a geochronological table and the textbook text, answer the questions and complete tasks on the contour map:

    What periods does the era cover?

    Duration of era

    What type of mountain building took place?

    What territories does the era cover?

    Designate the areas where these rocks are found

    What minerals are found

Defense of projects, discussion, distribution of points in the group: 1,2,3,4.

1. Pre-Paleozoic rocks (crystalline rocks: schists, gneisses - Tien-Shan village, Mugodzhary, Ulytau, Kokshetau).

2. Paleozoic sedimentary and igneous rocks (limestone, shale, sandstone - Tien-Shan village, Zhetysu Alatau, Tarbagatai, Altai; intrusions - copper, manganese, iron, tin, tungsten, gold).

3. Mesozoic rocks (Karatau, Pre-Uralsok plateau, Ileyskaya, Torgai depression).

4. Cenozoic rocks (throughout Kazakhstan):

A. Paleogene - basins: Shuiskaya, Ileyskaya, Zhaisan, plains - Ustirta, Aral region, Torgai plateau.

B. Neogene foothills of high mountain regions: sandy clays, loams.

B. Anthropogenic - everywhere.

Peer assessment - comment

Reception "Basket of Ideas"

Textbook

pp. 34 – 35

FO, mutual assessment

End of lesson 7-10 min

Individual work - test

    Do a test job

1. How many eras are there in the development of our Earth?

A) 6; B) 5; AT 3; D) 4

2. How many periods are there in the development of the Earth?

A)12; B) 14; AT 6; D) 10

3.Which era in the history of the Earth was the longest?

A) Paleozoic; B) Proterozoic; B) Archean

4.The first organisms arose in:

A) soil; B) air; In water.

5. When did mammals appear on Earth?

A) Proterozoic; B) Paleozoic; B) Mesozoic.

6. The appearance of primitive birds is the time:

A) Proterozoic; B) Paleozoic; B) Kainaza.

7. In what era and period were the first deserts formed on Earth?

A) Paleozoic; B) Cenozoic; B) Mesozoic;

D) Devonian; D) Perm; E) Jurassic

8.When did the first man appear?

A) Cenozoic era; Quaternary period;

B) Paleozoic era; Permian period;

B) Cenozoic era; Paleogene period

9. The most ancient folding on earth was formed in:

A) Archean era; B) Proterozoic era;

B) Paleozoic era.

10.Which minerals were the first to form on Earth?

A) Oil; B) Iron ore; B) Coal.

Peer review

1-b, 2-a, 3-c, 4-c, 5-c, 6-b, 7-d, 8-a, 9-a, 10-b

Grading

13 – 14 – “5”

12 – 10 – “4”

9 – 7 – “3”

Reflection “Boats at Sea”

Differentiation - How do you plan to support students?

How do you plan to encourage bright students?

Assessment - How do you plan to check student learning?

Health and safety precautions.

Reflections

Were the lesson/learning objectives realistic? What did students learn today? What was the atmosphere in the class? Did the differentiation I made work? Was the training time maintained? What deviations were there from the lesson plan and why?

final grade

Which two aspects of the learning went very well (in terms of teaching and learning)?

What two things could improve the lesson (taking into account teaching and learning)?

What did you learn about students as a whole or individuals?

“Checked” _________________ Short-term geography lesson plan 8.2.1.1. Lesson No. Class 8 Lesson topic: Purpose: Educational objectives: date 9 Geological chronology To study the features of geological chronology To form knowledge about the absolute and relative age of rocks. Reveal the structure of the geochronological table. Develop skills and abilities to work with a geochronological table. Develop analytical thinking and the ability to express your own opinion. Values ​​based on the national idea “Mangilik El”: Foster an active life position Studying new material Frontal, collective, group individual Instilling values ​​Lesson type Forms Methods Modules Equipment and visual aids: Expected result Working with terms and concepts Geographical objects: Lesson stages Beginning of the lesson 7 10 min Verbal, visual, reproductive New approaches, RCM, ICT, ODO, ROiT, LU, VO Physical map, tectonic map, geological map, geochronological table PC - presentation “Geological chronology” All students will be able to name: 1. Stages of the development of the Earth : planetary and geological. 2. Methods for determining the age of rocks. 3. Eras of Earth's development Most students will be able to use a geochronological table. Correlate eras and periods of duration Some students will be able to talk about the patterns of geological processes, work with the geochronological table Geology, tectonics, earth's crust, lithosphere, eras, periods, folding, plates and platforms, relief formation Russian platform, Turanian plate, Gondwana, Laurasia Lesson progress. Planned activities Resources I. Organizational moment. Organization of optimal conditions for educational activities. Checking student attendance. II. Activation of cognitive activity 1. What is the name of the country in which we live 2. What continent is Kazakhstan located on 3. In what part of the Eurasian continent is Kazakhstan located 4. What states does Kazakhstan border with 5. What landforms predominate in the "Pass" ball technique

Kazakhstan 6. In what part of Kazakhstan are the mountains located? 7. Name the highest peak of Kazakhstan 8. Name the lowest point of Kazakhstan 9. What large plains do you know. 10. What mountain ranges are there in Kazakhstan III. Watch the video “history of the earth in 5 minutes” Statement of the problem situation: IV. PC video Mid-lesson 2025 min Is the appearance of the earth's surface of our country, its nature, random? Have they always been like this? If not, how and why did they change? How did scientists prove that nature was constantly changing and developing? We have to answer these questions. Be careful. 1. Introduction “People guessed that the nature of the Earth was not always the way people see it when they encountered fossils, plants and animals that no longer exist, and shells. Gradually, the science of ancient life—paleontology—was formed. What are the names of scientists involved in this science? For many years, scientists around the world have been studying the preserved remains of animals and plants found in strictly defined layers of rocks. This means that the development of nature is inextricably linked with geological development, so they must be considered in unity. Currently, scientists have reconstructed a picture of the Earth's past by creating a geochronological table. Determining the age of rocks allows us to establish the relative and absolute time that has passed since some moment or event in the history of the Earth. If the occurrence of rocks is not disturbed, then each layer is younger than the one on which it lies. The topmost layer was formed later than all those lying below. The time during which each group of rocks accumulated is called an era. The name of the era reflects relative time - How is the absolute age of rocks determined? Absolute age is the time elapsed since the rock was formed. It is determined by radioactive elements - for example, uranium. The rate of its decay is known and always remains

Technique “Basket of Ideas” Textbook pp. 34 – 35 FO, mutual assessment of the constant (uranium decays into helium and lead, helium is seeded, lead remains) by the amount of lead determine the age of the rock Conclusion: Rocks are witnesses to the evolution of life 2. Working with geochronological table page 3435 Individual work turns into group work: students write down everything they know on this topic, or can extract from the table: Which columns stand out in it? Read the names of the periods of each era from the oldest to the youngest. What was the longest era in Earth's history? Which periods were the longest? Which period is the shortest? What changes occurred in nature in each era? What is the name of the era and period in which we live? They exchange baskets, read and discuss. 3. Group work 1st group – Archean and Proterozoic era 2nd group – Paleozoic era 3rd group – Mesozoic era 4th group – Cenazoic era Using atlas maps, geochronological table and textbook text, answer the questions and complete tasks on the contour map: 1. What periods covers the era 2. Duration of the era 3. What mountain building took place 4. What territories does the era cover 5. Designate the territories where these rocks are found 6. What minerals are found Defense of projects, discussion, distribution of points in the group: 1,2,3,4. 1. Pre-Paleozoic rocks (crystalline rocks: schists, gneisses - Tien-Shan village, Mugodzhary, Ulytau, Kokshetau). 2. Paleozoic sedimentary and igneous rocks (limestone, shale, sandstone - Tien-Shan village, Zhetysu Alatau, Tarbagatai, Altai; intrusions - copper, manganese, iron, tin, tungsten, gold). 3. Mesozoic rocks (Karatau, Pre-Uralsok

End of lesson 7 10 min plateau, Ileyskaya, Torgai depression). 4. Cenozoic rocks (throughout Kazakhstan): A. Paleogene - basins: Shuiskaya, Ileiskaya, Zhaisanskaya, plains - Ustirta, Aral Sea region, Torgai plateau. B. Neogene foothills of high mountain regions: sandy clays, loams. B. Anthropogenic - everywhere. Peer assessment comment Individual work - test 1. Complete test work 1. How many eras are there in the development of our Earth? A) 6; B) 5; AT 3; D) 4 2. How many periods are there in the development of the Earth? A)12; B) 14; AT 6; D) 10 3.Which era in the history of the Earth was the longest? A) Paleozoic; B) Proterozoic; B) Archean 4. The first organisms arose in: A) soil; B) air; In water. 5. When did mammals appear on Earth? A) Proterozoic; B) Paleozoic; B) Mesozoic. 6. The appearance of primitive birds is the time: A) Proterozoic; B) Paleozoic; B) Kainaza. 7. In what era and period were the first deserts formed on Earth? A) Paleozoic; B) Cenozoic; B) Mesozoic; D) Devonian; D) Perm; E) Jurassic 8. When did the first man appear? A) Cenozoic era; Quaternary period; B) Paleozoic era; Permian period; B) Cenozoic era; Paleogene period 9. The most ancient folding on earth was formed in: A) the Archean era; B) Proterozoic era; B) Paleozoic era. which 10. Select minerals were the first to form on Earth? A) Oil; B) Iron ore; B) Coal. Peer review 1b, 2a, 3c, 4c, 5c, 6 b, 7d, 8a, 9a, 10b Giving marks 13 – 14 – “5”

12 – 10 – “4” 9 – 7 – “3” Reflection “Boats in the Sea” Differentiation How do you plan to support students? How do you plan to encourage bright students? Assessment How do you plan to assess student learning? Health and safety precautions. Reflection Were the lesson/learning objectives realistic? What did students learn today? What was the atmosphere in the class? Did the differentiation I made work? Was the training time maintained? What deviations were there from the lesson plan and why? Final assessment Which two aspects of the learning went very well (taking into account teaching and learning)? 1 2 What two circumstances could improve the lesson (taking into account teaching and learning)? 1 2 What did you learn about students as a whole or individuals? 12