Ch 5 (50%)

42
Ch 5 Natural phenomena and disaster

Transcript of Ch 5 (50%)

Page 1: Ch 5 (50%)

Ch 5Natural phenomena and disaster

Page 2: Ch 5 (50%)

Geological disaster

Page 3: Ch 5 (50%)

Geology

• The science comprising the study of solid earth, the rocks of which it is composed, and the processes by which they change.

Page 4: Ch 5 (50%)

Why should we study geology?

Page 5: Ch 5 (50%)

>>to protect from the geological disaster...

Page 6: Ch 5 (50%)

What happened in 5 May 2014 in Chiang Rai?

• clip

Page 7: Ch 5 (50%)
Page 8: Ch 5 (50%)
Page 9: Ch 5 (50%)

11 march 2010 ... In Japan

Page 10: Ch 5 (50%)
Page 11: Ch 5 (50%)
Page 12: Ch 5 (50%)

26 December 2004

Page 13: Ch 5 (50%)

clip

Page 14: Ch 5 (50%)

>> for knowledge of mineral resources

Tin & Tungsten

• Found in the valleys along the granite mountains along the west of the country

Page 15: Ch 5 (50%)

Copper & Iron

• Found in Loei, Nong Khai, Uttaradit

Gold

• Chae Hom, Wang Nuea(Lampang)

• Mae Chan, Mae Sai and Chiang Saen (Chiang Rai)

Page 16: Ch 5 (50%)

>> for knowledge about how to manage the land

Page 17: Ch 5 (50%)

Why does rice grow better in water?

• Most types of rice require moist growing conditions so they cannot grow in areas of low rainfall unless the rice field is artificially irrigated. While rice needs water to grow, it does not require standing water to grow. The idea that rice needs to be grown in water is a misconception. However, rice is almost always grown in water filled fields, called paddies. While not required, there are benefits to the rice plant when grown in such conditions. Rice fields flood more easily than other row crop fields, because rice is grown in clay soils. Water does not readily drain through clay soil. Most other crops will not grow in this type of soil.

An advantage of this growing condition is weed control. Major plant cell functions like elongation and multiplication require oxygen. Flooded fields have less available oxygen for plant roots. This prevents the germination and growth of weeds that would compete with the rice plant for nutrients and sunlight in the field.

Standing water is also a deterrent to insects that threaten rice such as the army worm and chinch bug. Standing water also offers a kind of temperature control for the crop. Anyone who lives near a body of water knows that water temperature changes more slowly than land temperature. So, on hot days the water filled fields keep the rice cool, and then warm it on cool nights. Standing water also helps in preventing excessive salt accumulation and the soil depletion.

The interesting thing about rice is not that it grows in flooded fields, but that it can tolerate flooded conditions. Rice plant leaves and the stems contain a series of internal air tunnels that funnel air down to the roots. In this way it is similar to aquatic plants. One third of the rice plant needs to be above water for this mechanism to work. Rice that is totally under water will die. That is why the water level is carefully monitored and controlled in rice fields.

Page 18: Ch 5 (50%)

Geological study

>>Earth Materials

• Igneous rock,

• Sedimentary rock

• Metamorphic rock

clip

Page 19: Ch 5 (50%)

>> processes of earth change

Internal processes

By plate tectonics

– Divergent boundary, Convergent boundary, Transform fault boundary

Page 20: Ch 5 (50%)
Page 21: Ch 5 (50%)

External or Surficial processes

• Geologic processes acting on the surface of the solid earth in contact with the atmosphere and hydrosphere.

• Includes: Weathering, erosion, mass wasting, rivers and streams, glaciers, work of the wind, coastal processes, and groundwater.

Page 22: Ch 5 (50%)

Pothole?

Page 23: Ch 5 (50%)

a cavity or hole which appears to have been drilled in the surrounding rocks by eddying currents of water bearing stones, gravel and other detrital matter

Page 24: Ch 5 (50%)

>>> Geologic history

• follows the major events in Earth's past based on the geologic time scale, based on the study of the planet's rock layers

• Earth formed about 4.54

clip

Page 25: Ch 5 (50%)

How the earth was created?

Page 26: Ch 5 (50%)

Geological map

William Smith (Father of English Geoloy)

Page 27: Ch 5 (50%)

Geological map

• a special-purpose map to show geological features; i.e rock units, geological structures and ages, 3d-orientation, etc

Page 28: Ch 5 (50%)

>>> By Department of Geology, Department of Mineral Resources

• Determine the extent of the mineral

• coal and petroleum exploration (Aimed at exploring areas of the Tertiary rock era)

• Tin exploration (aimed at granite area)

Page 29: Ch 5 (50%)

• 66 million to 2.58 million years ago,

Page 30: Ch 5 (50%)

Structure geology

• the study of the three-dimensional distribution of rock units with respect to deformational histories (e.g., mountain building, rifting due to plate tectonics)

• To understand the dynamics of the stress field that can be linked to important events in the regional geologic past

Page 31: Ch 5 (50%)

Chiang Rai Geology

Page 32: Ch 5 (50%)
Page 33: Ch 5 (50%)

Active fault : a fault that is likely to have another earthquake sometime in the future. one that has ruptured in the last 11,000 years

Page 34: Ch 5 (50%)

Phu Chi Fa

• a mountain in located at the eastern edge of Thoeng district, Chiang Rai

Page 35: Ch 5 (50%)
Page 36: Ch 5 (50%)

Geohazards

• a geological state which has the potential to create widespread damage.• include tectonic issues, such as earthquakes and volcanoes• other naturally-occurring processes such as landslides and mud flows

Page 37: Ch 5 (50%)

earthquake

• a sudden release of energy in the Earth’s crust that creates waves

Page 38: Ch 5 (50%)

Landslide

• Gravity is the primary factor in a landslide. Soil on a flat surface does not move. On a slope, gravity alone also may not trigger a landslide. But when another disrupting factor -- like rain -- comes into play, gravity will pull sediment downhill.

Page 39: Ch 5 (50%)

What can be factors for lanslide?

Page 40: Ch 5 (50%)

Sinkhole

• A hole in the ground caused by some form of collapse of the surface layer.

• The most significant factor in the development of sinkholes is the dissolution of the limestone underlying by acidic waters.

Page 41: Ch 5 (50%)

Soil creep

• the slow downward progression of rock and soil down a low grade slope

Page 42: Ch 5 (50%)

Bank erosion

• the wearing away of the banks of a stream or river