Social Sciences, asked by manojjamatia66023, 8 months ago

describe the effects of the physical features​

Answers

Answered by yashikakushwaha2
0

Effects of physical features on human activities

Physical features are important to us because of the positive and negative effects they have on people’s lives.

Positive effects

1. Farming:

Volcanic mountains produce fertile volcanic soils, which are important for farming. Plateaus and plains are suitable for setting up large farms where machinery can be easily used.

2. Settlement:

In hot tropical areas, highlands have a cool and wet climate that attracts settlements.

Plains attract settlements because they can easily be irrigated to grow different crops.

3. Water supply:

Mountains are sources of rivers, which supply water for domestic and industrial use.

Rivers also provide water for irrigation.

4. Rainfall:

When warm moist winds rise over mountains, they form relief rainfall. Highland areas receive this type of rainfall.

5. Security:

Highland areas offer security to the people living there. In the past, people used to settle in highland areas to feel safe.

They would see their enemies approaching and prepare to defend themselves.

6. Borders:

Mountains, rivers and lakes are used as boundaries between countries.

7. Tourist attraction:

Relief features form beautiful scenery, which attracts tourists.

Examples of such features include the snow-capped mountains, the Great Rift Valley and lakes.

Tourists bring foreign exchange into the country.

8. Transport:

Lakes and rivers are used as a means of transport.

For example, Lake Victoria is an important waterway which links Kenya, Uganda and Tanzania. Lake Tanganyika is also used for transport.

9. Fishing:

Many lakes and rivers have fi sh.

Fish is an important source of food that is rich in proteins.

Fishing earns income for many families living near the lakes and rivers.

10. Mining:

The earth is a source of useful and valuable minerals like gold, diamond and oil.

Lakes like L. Magadi are important sources of minerals like salt and soda ash.

11. Recreation:

People climb mountains and hills for enjoyment.

Rivers, lakes and the ocean are used for water sports, swimming, and sailing.

12. Source of electricity:

Rivers and dams are used to generate electricity.

13. Communication:

Masts to improve communication are set up in highland areas to improve communication.

14. Livestock farming:

Dry plateaus like the Nyika plateau are good for keeping livestock and nomadic pastoralism.

15. Sources of rivers:

Mountains and highlands are sources of rivers since the ice melts to water.

16. Some lakes and rivers provide water for irrigation.

For example: L. Naivasha, R. Tana and L. Bogoria.

17. Some features in the Rift Valley are sources of minerals,

for example, salt and soda ash at L. Magadi and fl uorspar at Kerio Valley.

18. Forests found at the foot of high mountains and within the Rift Valley provide raw materials for some industries,

for example, wood and timber used in paper making industries and saw mills.

19. Forests are home to wild animals which attract tourists.

20. Steam from hot volcanic rocks within the Rift Valley is used to generate geothermal power, for example, at the Ol Karia Geothermal Plant near Naivasha.

Negative effects

1. Relief features affect the way people settle in different places.

For example, areas that are hilly, with steep rugged sides, will not support dense settlements.

2. Mountains may obstruct free movement of people from one place to another. It is diffi cult and expensive to build roads in such areas.

3. Lowland areas and swamps tend to fl ood and this may cause loss of lives and property.

4. Hot lava can also lead to destruction of property.

5. When lowland areas fl ood, they become breeding grounds for pests like mosquitoes and snails, which cause diseases.

Answered by Anonymous
0

Answer:

Habitat Harshness Hypothesis (HHH) and Habitat Safety Hypothesis (HSH) successfully predict trends in diversity, abundance, individual growth, survival rate, and reproductive success of intertidal and supralittoral macrofauna species according to beach morphodynamic states. However, the effects of beach physical features on secondary production are still poorly known, especially concerning the response of species that inhabit different beach zones. Here we tested the hypothesis that production and P/B ratio of common species of lower and middle intertidal, the wedge clam Donax hanleyanus and the isopod Excirolana armata, respectively, follow HHH, increasing towards less severe dissipative/intermediate conditions. Conversely, the turnover rate (production-to-biomass ratio: P/B) of both species is expected to increase towards harsher reflective conditions according to Allen's relationship (instantaneous mortality rate Z = P/B). On the other hand, the production and P/B of the supralittoral isopod Excirolana braziliensis are expected to follow HSH, i.e. an opposite pattern to that of intertidal species, with higher production on reflective beaches and higher P/B on dissipative ones. To test these predictions, relationships of production and P/B with physical characteristics of beaches (grain size, beach slope, and width) were assessed using 34 estimates gathered from literature, obtained from 14 microtidal beaches located in the Southwestern Atlantic coasts. The results showed that D. hanleyanus production increased towards dissipative conditions following HHH, although P/B ratio followed the production trend. These results, however, agree with those previously observed in the mole crab Emerita brasiliensis, reinforcing these trends for inhabitants of the swash zone, the harshest beach zone. Similarly, E. armata production increased sharply towards dissipative conditions, finer sand and gentler slopes, an expected pattern for a middle intertidal, highly-substrate specific species. Production and P/B of the supralittoral species E. braziliensis followed HHH rather than HSH, with higher production in intermediate/dissipative conditions, and inversely, higher P/B and Z on reflective beaches. This study shows that the production of intertidal species both in the lower and in the middle intertidal increases from reflective to intermediate/dissipative conditions.

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