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Neolithic Period (4200-2500 yrs ago)
Domesticating plants and animals and crafting better tools
Dynamic interplay between humans and environment
Austronesian-speaking
New Stone Age
Hydrometeorological Hazards
accidents by atmospheric, hydrological, or oceanographic nature
Western Pacific Basin
Most Active Tropical Cyclone Basin
Intertropical Convergence Zone (ITCZ)
Trade winds from North Hem n South Hem bring tropical air masses together
Formation of convective clouds and heavy precipitation
Typhoon
Revolves around low-pressure area
“Tai Fung” Ta big, Fung wind
“Bagyo”
Cyclone Classifications
Trop Depres - 61 kph
Trop Storm - 62 to 88 kph
Severe Trop Storm - 89 to 117 kph
Typhoon - 118 to 220 kph
Super Typhoon - >220 kph
Observance for DO 37
Cancellation of Public Schools
Thunderstorm
Lightning and Thunder
Formation of Thunderstorm
Moisture
Rapid rising mass of warm air
Updraft to force moisture higher
Flood
excessive water
Storm Surge
“Daluyong ng Bagyo”
drop in atmospheric pressure and strong winds
ABNORMAL SEAWATER LEVEL RISE
El Nino
“Christ Child” Unusual warming of ocean waters
Dry
La Nina
“The Girl” unusual cooling of sea
wet
Landslide
downard movement of soil
southwest monsoons (habagat)
sinkholes
depressions or holes”
“karst terrains” - area where soil can easily be dissolved
Translational Landslide
along parallel surface
Rotational Landslide
Ground rotates
Block slide
one block falls
Topple
piece of cliff falling
earthflow
hourglass slope
debris flow
with rain and soil slope flow
debris avalanche
mas malala na debris flow
lateral spread
spreading of materials on floor
Tsunami
tidal waves, huge waves
Erosion
rock particles worn away and moved somewhere else by a transporr agent
Natural Causes of Erosion
Heavy Rainfall
Wind
Soil Erodibility
Local Climate
Vegetation Loss
Human Causes of Erosion
Mining
Deforestation
Shifting Agriculture
Saltwater Intrusion
Seawater infiltrates freshwater aquifers
contaiminating fresh water supply
human activties like groundwater exrraction and construction