Tuesday, July 23, 2019

PDRRMO's Response Capacity

  • 20170907_112000.jpg
  • 20170907_112027.jpg
  • 20170907_112058.jpg
  • 20170907_112138.jpg
  • 20170907_112149.jpg
  • 20170908_170256.jpg
  • 20180110_084349.jpg
  • 20180117_142735.jpg
  • 20180117_142812.jpg
  • 23622326_1983588738321444_7471660543091984425_n.jpg
  • Sea_Ambulance.JPG

PDRRMC's Dredging Equipment now Operational

flood controlOn April 17, 2018, personnel from the Provincial Engineering Office (PEO) had successfully loaded the back hoe onto the newly completed barge, a part of the dredging equipment package project of the Provincial Disaster Risk Reduction and Management Council (PDRRMC) at the Pansipit River.

The self-sustaining barge was constructed in San Nicolas, Batangas earlier.  The dredging equipment package comes with a backhoe, a bin loader and dump truck.  The PDRRMC project aimed to ease and dregde most water bodies in the province toflood control project avoid heavy flooding during rainy season and at the same time, to provide immediate assistance to local governments in the province that may need its services.

Photo and video taken by Engr. Ethel Arellano during the actual loading operations at the Pansipit River.

MOA with NFA

The Provincial Disaster Risk Reduction and Management Council (PDRRMC) MOA Signingand the National Food Authority (NFA) entered into an agreement that the former shall procure rice from the latter in times of calamities in the province of Batangas.  The signing of the Memorandum of Agreement (MOA) was highlighted during the 2018 1st Quarter PDRRM full Council Meeting last April 4, 2018.

Hon. Hermilando I. Mandanas, Governor and Chairperson of the PDRRMC represented the provincial government while Mr. Miguel S. Tecson, Provincial Manager, signed in behalf of the National Food Authority.  

Gov. Mandanas stressed that everytime a calamity affects our province, our people's concern is for food, particularly rice.  The Governor appreciated the efforts of the National Food Authority to support the province of Batangas for cheaper price of rice.  Although we have enough supply of rice in the province due to supply of our neigboring provinces like Mindoro.  He further reported that the rice production of Batangas Province is less than 20% of its actual consumption.

Full context of this MOA shall be uploaded under the "About PDRRMO" menu soon.

PDRRMO Staff Underwent Radio Operators Training

20180326 102845

Batangas City.  Employees and staff of the Batangas Provincial Disaster Risk Reduction and Management Office underwent a 1-day training for radio operations (Restricted Radio Telephone Operator for Land Mobile or RLM on a Commercial Service) on Monday, March 26, 2018 at the PDRRM office at the Provincial Sports Complex in Barangay Bolbok, Batangas City.

Attendees on the said training were briefed on the laws and regulations concerning the use of 2-way radios (portable or handheld, land mobile or vehicle mounted and base radio) by Engr. Jasmine Rapada of the National Telecommunications Commission Region IV.

"This training was aimed to provide licenses to PDRRMO operatives for using portable radios during times of distress and to ensure that the PDRRMO abides by all rules and regulations applicable and being enforced by the NTC", said Mr. Joselito M. Castro, Provincial Disaster Risk Reduction and Management Officer of the Batangas Province.

for news

Role of Media in Disaster Management

Batangas City.  The Provincial Disaster Risk Reduction and Management Office (PDRRMO) conducted a 1-day seminar workshop dubbed as the "Role of Media in Disaster Management" on December 19, 2017 at the  DepEd Conference Hall, Batangas Provincial Sports Complex in Brgy. Bolbok, this city.  

In his welcome and opening remarks, Mr. Joselito M. Castro stressed the importance of media in disaster operations not only in information dissemination, but also for the swift and orderly management of disasters.

Resource speakers for the activity were Ms. Georgina R. Garcia of the Office of Civil Defense IV-A and Mr. Antonio V. de Lacy, Jr. of the Provincial Disaster Risk Reduction and Management Office of Batangas.

The event was participated by representatives from both print and broadcast media based in Batangas as well as personnel from the Provincial Information Office.

Batangas Local DRRMOs in Taal

2018 1st Qtr NSED in Rosario

Emergency Medical Services

Weather Forecast

Daily Weather Forecast (Southern Luzon)

Issued at:4:00 AM today, 10 June 2018 

SYNOPSIS: As of 3:00am  today, the center of Severe  Tropical Storm "DOMENG" {MALIKSI}  was estimated, based on all available data at 855  km East Northeast of Basco, Batanes  (23.9 ºN, 129.4 ºE) with maximum sustained winds of  100 km/h near the center and gustiness of up to 120 km/h. It is forecast to move Northeast at  32 km/h. Southwest  Monsoon affecting Luzon and Visayas.










Severe Weather Bulletin

FOR:Typhoon Domeng 
Tropical Cyclone: ALERT 

ISSUED AT:9:30 AM, 10 June 2018 


  • The Southwest Monsoon (Habagat) enhanced by the Typhoon will continue bringing monsoon rains over Luzon, especially over the western section, until early next week. The public is advised to continue monitoring for updates, take appropriate actions against possible flooding and landslides, and coordinate with local disaster risk reduction and management offices.
  • Sea travel remains risky over the northern and eastern seaboards of Northern Luzon, the seaboards of Central Luzon, and the western and southern seaboards of Southern Luzon.

Earthquake Bulletin

On June 10, 2018, at about 4:10 A.M., a magnitude 2.6 earthquake hit Calatagan, Batangas with the following data:

Latitude (oN):       13.63

Longtitude (oE):   120.64

Depth:                  89 KM

Epicenter:             022 km S 01° E of Calatagan (Batangas)

Source:                 www.phivolcs.dost.gov.ph






Onset of the Rainy Season 2018

The occurrence of widespread rainfall recorded in most PAGASA stations during the past few days due to the southwest monsoon (“Habagat”) confirms the onset of the rainy season over the western part of the country. These areas, including Metro Manila, will continue to experience scattered to widespread rains and thunderstorms in the coming days. However, such rain events may be followed by dry periods (also known as a “monsoon break”) that could last for several days to two weeks. 

PAGASA will continue to closely monitor the situation, and updates/advisories shall be issued as appropriate. The public and all concerned agencies are advised to take precautionary measures against the impacts of the rainy season. 

For further information, please contact PAGASA at telephone numbers 927-1335 or 434-0955.

  • Emergency Response Preparedness Meeting for TS Urduja 12 14 2017

    Batangas City.  The Provincial Disaster Risk Reduction and Management Council (PDRRMC) conducted an emergency preparedness meeting for Tropical Storm "Urduja" on December 14, 2017, should the said weather disturbance affect the province.  Presided over by Acting Governor Sofronio "Nas" Ona and assisted by PDRRM Officer Joselito M. Castro, members of the Council attended the meeting that took place at the Provincial Disaster Risk Reduction and Management Office at the Provincial Sports Complex, Brgy. Bolbok, this city.

What is Vehicle Extrication?

VexPixVehicle extrication is the process of removing a vehicle from around a person who has been involved in a motor vehicle accident, when conventional means of exit are impossible or inadvisable. A delicate approach is needed to minimize injury to the victim during the extrication. This operation is typically accomplished by using chocks and bracing for stabilization and hydraulic tools, including the Jaws of Life.

The basic extrication process consists of, but is not limited to, six steps:

  • the protection of the accident scene, to avoid a risk of another collision (marking out the scene with cones or flares (not advisable if gasoline is leaking), lighting) and of fire (e.g. switching off the ignition, putting vehicle in park, disconnecting the battery, placing absorbing powder on oil and gasoline pools, fire extinguisher and fire hose ready to use);
  • patient triage and initial medical assessment of the patient by a qualified medical rescuer;
  • securing the vehicle to prevent the unexpected movement (e.g. falling in a ditch), and the movements of the suspension, either of which could cause an unstable trauma wound or cause injury to the rescuers; a vehicle should never be moved, it should always be secured.
  • the opening of the vehicle and the deformation of the structure (such as removing a window) to allow the intervention of a first responder, of a paramedic or of a physician inside the vehicle to better assess the patient and begin care and also to release a possible pressure on the casualty;
  • removal of a section of the vehicle (usually the roof or door) to allow for safe removal of the accident victim, especially respecting the head-neck-back axis (rectitude of the spine);
  • removal of the person from the vehicle

In less complicated cases, it is possible to extricate the casualty without actually cutting the vehicle, such as removing a person from the side door or another part of the vehicle.

As soon as possible, best before beginning the mechanical operation, a medically trained person enters the cabin to perform first aid on the casualty: mid-level assessment, stopping the bleeding, putting a cervical collar on the patient (extrication operations are likely to provoke vibrations), providing oxygen first aid. In France, this rescuer is called the "squirrel" (écureuil). NFPA regulation 1006 and 1670 state that all "rescuers" must have medical training to perform any technical rescue operation, including cutting the vehicle itself. Therefore, in almost all rescue environments, whether it is an EMS Department or Fire Department that runs the rescue, the actual rescuers who cut the vehicle and run the extrication scene are Medical First Responders, Emergency Medical Technicians, or Paramedics, as a motor vehicle accident has a patient involved.

After the vehicle has been secured and access gained to the patient, the EMS team then enters to perform more detailed medical care. Continued protection of the patient from extrication itself, using hard and soft protection, should be done at all times. The deformation of the structure and the section of the roof take several minutes; this pre-extrication time can be used for medical or paramedical acts such as intubation or placing an intravenous drip. When the casualty is in cardiac arrest, cardiopulmonary resuscitation can be performed during the freeing, the casualty being seated. The use of this incompressible duration is sometimes called play and run, as a compromise between scoop and run (fast evacuation to a trauma center) and stay and play (maximum medical care onsite).

The last step is usually performed with a long spine board: the casualty is pulled up on it. An extrication splint (KED) can help to immobilise the spine during this operation.

FEATURE:  11 Facts about Volcanoes


  1. A volcano is a mountain that opens downward to a pool of molten rock below the surface of the earth. When pressure builds up, eruptions occur.
  2. In an eruption, gases and rock shoot up through the opening and spill over or fill the air with lava fragments. Eruptions can cause lava flows, hot ash flows, mudslides, avalanches, falling ash and floods.
  3. The danger area around a volcano covers about a 20-mile radius.
  4. Fresh volcanic ash, made of pulverized rock, can be harsh, acidic, gritty, glassy and smelly. The ash can cause damage to the lungs of older people, babies and people with respiratory problems.
  5. Volcanic lightning occurs mostly within the cloud of ash during an eruption, and is created by the friction of the ash rushing to the surface. Roughly 200 accounts of this lightning have been witnessed live.
  6. An erupting volcano can trigger tsunamis, flash floods, earthquakes, mudflows and rockfalls.
  7. More than 80% of the earth's surface is volcanic in origin. The sea floor and some mountains were formed by countless volcanic eruptions. Gaseous emissions from volcano formed the earth's atmosphere.
  8. There are more than 500 active volcanoes in the world. More than half of these volcanoes are part of the "Ring of Fire," a region that encircles the Pacific Ocean.
  9. Active volcanoes in the U.S. are found mainly in Hawaii, Alaska, California, Oregon and Washington, but the greatest chance of eruptions near areas where many people live is in Hawaii and Alaska.
  10. The sound of an eruption volcano can be quiet and hissing or explosive and booming. The loud cracks travel hundreds of miles and do the most damage, including hearing loss and broken glass.
  11. The most deadly eruptions have occurred in Indonesia, with tens of thousands of lives lost to starvation, tsunami (as a result of the eruption), ash flows, and mudflows.


What Are The Benefits Of Volcanoes?

Article written: 19 March, 2016
Updated: 4 May, 2017

by Matt Williams

Volcanoes are renowned for their destructive power. In fact, there are few forces of nature that rival their sheer, awesome might, or have left as big of impact on the human psyche. Who hasn’t heard of tales of Mt. Vesuvius erupting and burying Pompeii? There’s also the Minoan Eruption, the eruption that took place in the 2nd millennium BCE on the isle of Santorini and devastated the Minoan settlement there.

In Japan, Hawaii, South American and all across the Pacific, there are countless instances of eruptions taking a terrible toll. And who can forget modern-day eruptions like Mount St. Helens? But would it surprise you to know that despite their destructive power, volcanoes actually come with their share of benefits? From enriching the soil to creating new landmasses, volcanoes are actually a productive force as well.

Soil Enrichment:

Volcanic eruptions result in ash being dispersed over wide areas around the eruption site. And depending on the chemistry of the magma from which it erupted, this ash will be contain varying amounts of soil nutrients. While the most abundant elements in magma are silica and oxygen, eruptions also result in the release of water, carbon dioxide (CO²), sulfur dioxide (SO²), hydrogen sulfide (H²S), and hydrogen chloride (HCl), amongst others.

In addition, eruptions release bits of rock such as potolivine, pyroxene, amphibole, and feldspar, which are in turn rich in iron, magnesium, and potassium. As a result, regions that have large deposits of volcanic soil (i.e. mountain slopes and valleys near eruption sites) are quite fertile. For example, most of Italy has poor soils that consist of limestone rock.

But in the regions around Naples (the site of Mt. Vesuvius), there are fertile stretches of land that were created by volcanic eruptions that took place 35,000 and 12,000 years ago. The soil in this region is rich because volcanic eruption deposits the necessary minerals, which are then weathered and broken down by rain. Once absorbed into the soil, they become a steady supply of nutrients for plant life.

Hawaii is another location where volcanism led to rich soil, which in turn allowed for the emergence of thriving agricultural communities. Between the 15th and 18th centuries on the islands of Kauai, O’ahu and Molokai, the cultivation of crops like taros and sweet potatoes allowed for the rise of powerful chiefdoms and the flowering of the culture we associate with Hawaii today.

Volcanic Land Formations:

In addition to scattering ash over large areas of land, volcanoes also push material to the surface that can result in the formation of new islands. For example, the entire Hawaiian chain of islands was created by the constant eruptions of a single volcanic hot spot. Over hundreds of thousands of years, these volcanoes breached the surface of the ocean becoming habitable islands, and rest stops during long sea journeys.

This is the case all across the Pacific, were island chains such as Micronesia, the Ryukyu Islands (between Taiwan and Japan), the Aleutian Islands (off the coast of Alaska), the Mariana Islands, and Bismark Archipelago were all formed along arcs that are parallel and close to a boundary between two converging tectonic plates.

The island of Santorini, Greece. Credit: EOS/NASA/ Public Domain

Much the same is true of the Mediterranean. Along the Hellenic Arc (in the eastern Mediterranean), volcanic eruptions led to the creation of the Ionian Islands, Cyprus and Crete. The nearby South Aegean Arc meanwhile led to the formation of Aegina, Methana, Milos, Santorini and Kolumbo, and Kos, Nisyros and Yali. And in the Caribbean, volcanic activity led to the creation of the Antilles archipelago.

Where these islands formed, unique species of plants and animals evolved into new forms on these islands, creating balanced ecosystems and leading to new levels of biodiversity.

Volcanic Minerals and Stones:

Another benefits to volcanoes are the precious gems, minerals and building materials that eruptions make available. For instance, stones like pumice volcanic ash and perlite (volcanic glass) are all mined for various commercial uses. These include acting as abrasives in soaps and household cleaners. Volcanic ash and pumice are also used as a light-weight aggregate for making cement.

The finest grades of these volcanic rocks are used in metal polishes and for woodworking. Crushed and ground pumice are also used for loose-fill insulation, filter aids, poultry litter, soil conditioner, sweeping compound, insecticide carrier, and blacktop highway dressing.

The roof of the Pantheon, as seen from nearby rooftops in Roe. Credit: Public Domain/Anthony Majanlahti

Perlite is also used as an aggregate in plaster, since it expands rapidly when heated. In precast walls, it too is used as an aggregate in concrete. Crushed basalt and diabase are also used for road metal, railroad ballast, roofing granules, or as protective arrangements for shorelines (riprap). High-density basalt and diabase aggregate are used in the concrete shields of nuclear reactors.

Hardened volcanic ash (called tuff) makes an especially strong, lightweight building material. The ancient Romans combined tuff and lime to make a strong, lightweight concrete for walls, and buildings. The roof of the Pantheon in Rome is made of this very type of concrete because it’s so lightweight.

Precious metals that are often found in volcanoes include sulfur, zinc, silver, copper, gold, and uranium. These metals have a wide range of uses in modern economies, ranging from fine metalwork, machinery and electronics to nuclear power, research and medicine. Precious stones and minerals that are found in volcanoes include opals, obsidian, fire agate, flourite, gypsum, onyx, hematite, and others.

Global Cooling:

Volcanoes also play a vital role in periodically cooling off the planet. When volcanic ash and compounds like sulfur dioxide are released into the atmosphere, it can reflect some of the Sun’s rays back into space, thereby reducing the amount of heat energy absorbed by the atmosphere. This process, known as “global dimming”, therefore has a cooling effect on the planet.

Sarychev volcano, (located in Russia’s Kuril Islands, northeast of Japan) in an early stage of eruption on June 12, 2009. Credit: NASA

The link between volcanic eruptions and global cooling has been the subject of scientific study for decades. In that time, several dips have been observed in global temperatures after large eruptions. And though most ash clouds dissipate quickly, the occasional prolonged period of cooler temperatures have been traced to particularly large eruptions.

Because of this well-established link, some scientists have recommended that sulfur dioxide and other be released into the atmosphere in order to combat global warming, a process which is known as ecological engineering.

Hot Springs and Geothermal Energy:

Another benefit of volcanism comes in the form of geothermal fields, which is an area of the Earth characterized by a relatively high heat flow. These fields, which are the result of present, or fairly recent magmatic activity, come in two forms. Low temperature fields (20-100°C) are due to hot rock below active faults, while high temperature fields (above 100°C) are associated with active volcanism.

Geothermal fields often create hot springs, geysers and boiling mud pools, which are often a popular destination for tourists. But they can also be harnessed for geothermal energy, a form of carbon-neutral power where pipes are placed in the Earth and channel steam upwards to turn turbines and generate electricity.

Steam rising from the Nesjavellir Geothermal Power Station in Iceland. Credit: Gretar Ívarsson/Fir0002

In countries like Kenya, Iceland, New Zealand, the Phillipines, Costa Rica and El Salvador, geothermal power is responsible for providing a significant portion of the country’s power supply – ranging from 14% in Costa Rica to 51% in Kenya. In all cases, this is due to the countries being in and around active volcanic regions that allow for the presence of abundant geothermal fields.

Outgassing and Atmospheric Formation:

But by far, the most beneficial aspect of volcanoes is the role they play in the formation of a planet’s atmosphere. In short, Earth’s atmosphere began to form after its formation 4.6 billion eyars ago, when volcanic outgassing led to the creation of gases stored in the Earth’s interior to collect around the surface of the planet. Initially, this atmosphere consisted of hydrogen sulfide, methane, and 10 to 200 times as much carbon dioxide as today’s atmosphere.

After about half a billion years, Earth’s surface cooled and solidified enough for water to collect on it. At this point, the atmosphere shifted to one composed of water vapor, carbon dioxide and ammonia (NH³). Much of the carbon dioxide dissolved into the oceans, where cyanobacteria developed to consume it and release oxygen as a byproduct. Meanwhile, the ammonia began to be broken down by photolysis, releasing the hydrogen into space and leaving the nitrogen behind.

Another key role played by volcanism occurred 2.5 billion years ago, during the boundary between the Archaean and Proterozoic Eras. It was at this point that oxygen began to appear in our oxygen due to photosynthesis – which is referred to as the “Great Oxidation Event”. However, according to recent geological studies, biomarkers indicate that oxygen-producing cyanobacteria were releasing oxygen at the same levels there are today. In short, the oxygen being produced had to be going somewhere for it not to appear in the atmosphere.

Roughly 2.5 billion years ago, towards the end of the Archaean Era, oxidation of our atmosphere began. Credit: ocean.si.edu

The lack of terrestrial volcanoes is believed to be responsible. During the Archaean Era, there were only submarine volcanoes, which had the effect of scrubbing oxygen from the atmosphere, binding it into oxygen containing minerals. By the Archaean/Proterozoic boundary, stabilized continental land masses arose, leading to terrestrial volcanoes. From this point onward, markers show that oxygen began appearing in the atmosphere.

Volcanism also plays a vital role in the atmospheres of other planets. Mercury’s thin exosphere of hydrogen, helium, oxygen, sodium, calcium, potassium and water vapor is due in part of volcanism, which periodically replenishes it. Venus’ incredibly dense atmosphere is also believed to be periodically replenished by volcanoes on its surface.

And Io, Jupiter’s volcanically active moon, has an extremely tenuous atmosphere of sulfur dioxide (SO²), sulfur monoxide (SO), sodium chloride (NaCl), sulfur monoxide (SO), atomic sulfur (S) and oxygen (O). All of these gases are provided and replenished by the many hundreds of volcanoes situated across the moon’s surface.

As you can see, volcanoes are actually a pretty creative force when all is said and done. In fact, as terrestrial organisms depend on them for everything from the air we breathe, to the rich soil that produces our food, to the geological activity that gives rise to terrestrial renewal and biological diversity.


3023455 poster p volcano

Hazardous Volcanic Events

There are several kinds of events caused from volcanic action that can be harmful to life and property. These include lava flows, lahars, ash falls, debris avalanches, and pyroclastic density currents.

Pyroclastic Density Currents

Pyroclastic density currents are are gravity-driven, rapidly moving, ground-hugging mixtures of rock fragments and hot gases. This mixture forms a dense fluid that moves along the ground with an upper part that is less dense as particles fall toward the ground. The behavior of the fluid depends upon the solids concentration relative to the amount of hot gases (i.e., solids-gas ratio). High concentration density flows are called "pyroclastic flows" and are essentially nonturbulent and confined to valleys. Low concentration density flows are called "pyroclastic surges" which can expand over hill and valley like hurricanes. Temperatures may be as hot as 900 degrees Celsius, or as cold as steam ( see "base surges" in section on Hydroclastic Processes).

Pyroclastic flows and surges are potentially highly destructive owing to their mass, high temperature, high velocity and great mobility. Deadly effects include asphyxiation, burial, incineration and crushing from impacts. Many people and the cities of Pompeii and Herculaneum were destroyed in 79 AD from an erupion of Mount Vesuvius; 29,000 people were destroyed by pyroclastic surges at St. Pierre, Martinique in 1902; >2000 died at Chichónal Volcano in southern Mexico in 1982 from pyroclastic surges. The only effective method of risk mitigation is evacuation prior to such eruptions from areas likely to be affected by pyroclastic density currents.


Lahars are part of the family of debris flows that are fluids composed of mixtures of water and particles of all sizes from clay-size to gigantic boulders. The abundance of solid matter carries the water, unlike watery floods where water carries the fragments. Debris flows have the viscous consistency of wet concrete, and there is a complete transition to watery floods. Lahars are composed of volcanic particles and originate directly or indirectly from volcanic action. Lahars can form by hot pyroclastic surges or flows entering watershed systems or flowing over snow and ice, by eruptions through crater lakes, by heavy rains on loose volcanic debris -- that is, any process by which volcanic particles can become saturated by water and move downslopes. They can move with velocities as low as 1.3 m/s to as great as 40 m/s on steep slopes (1 m/s = 2.55 miles per hour). They are known to have travelled as far as 300 km (1 km = 0.63 miles). Lahars have destroyed many villages and lives living on Indonesian volcanoes because most people live in valleys where lahars flow. The 21,000 lives lost at Armero, Colombia, was from a lahar that formed during the eruption of Nevado del Ruiz in 1985. It was generated by meltwater from the interaction of pyroclastic surges with snow and ice, from a very small eruption. Lahars can transform into regular floods as they become increasingly diluted with water downstream. This phenomenon was first discovered at Mount St. Helens where hot pyroclastic surges transformed to lahars, which further transformed to hyperconcentrated streamflow and then to normal stream-flow turbulence (floods).

Debris-flow Avalanches

The eruption of Mount St. Helens on May 18, 1980 started with a relatively small volcanic earthquake that caused collapse of the north side of the volcano because it was oversteepened and therefore unstable. When the landslide occurred, it decreased the pressure on the pressurized interior of the volcano which expanded explosively to form a lateral blast that devastated the countryside north of the volcano. Most of the debris flow avalanche was diverted down the North Fork Toutle River, but some moved directly northward over a 300 meter ridge and down into the next valley. Since the 1980 Mount St. Helens eruption, dozens of volcanoes that have given rise to avalanches have been discovered. For example, 40 avalanches exceeding 1 Km3 in volume, and 22 with a volume of less than 1 km3, are now known from the Quaternary alone, and 17 historic volcanic avalanches have been identified. The hilly topography north of Mount Shasta in northern California is now known to be the result of a have debris-flow avalanche. Some are known to extend up to 85 km from their sources and to cover tens to more than 1000 km2 in area.

Lava flows

Lava flows rarely threaten human life because lava usually moves slowly -- a few centimeters per hour for silicic flows to several km/hour for basaltic flows. An exceptionally fast flow (extremely rare) at Mt. Nyiragongo, Zaire (30-100 km/hour), overwhelmed about 300 people. Major hazards of lava flows -- burying, crushing, covering, burning everything in their path. Sometimes lava melts ice and snow to cause floods and lahars. Lava flows can dam rivers to form lakes that might overflow and break their dams causing floods. Methods for controlling paths of lava flows: (1) construct barriers and diversion channels, (2) cool advancing front with water, (3) disruption of source or advancing front of lava flow by explosives.

Tephra falls and Ballistic Projectiles formed on Land

Tephra consists of pyroclastic fragments of any size and origin. It is a synonym for "pyroclastic material." Tephra ranges in size from ash (<2 mm) to lapilli (2-64 mm) to blocks and bombs (>64 mm). Densities vary greatly, from that of pumice (<0.5)) to solid pieces of lava with density about 3.0. Blocks from basement material may exceed 3.0. Material may be juvenile (formed of magma involved in the eruption ) or accidental (derived from pre-existing rock).

Tephra fall and ballistic projectiles endanger life and property by (1) the force of impact of falling fragments, but this occurs only close to an eruption, (2) loss of agricultural lands if burial is greater than 10 cm depth, (3) producing suspensions of fine-grained particles in air and water which clogs filters and vents of motors, human lungs, industrial machines, and nuclear power plants, and (4) carrying of noxious gases, acids, salts, and, close to the vent, heat. Burial by tephra can collapse roofs of buildings, break power and communication lines and damage or kill vegetation. Even thin (<2 cm) falls of ash can damage such critical facilities as hospitals, electic-generating plants, pumping stations, storm sewers and surface-drainage systems and sewage treatment plants, and short circuit electric-transmission facilities, telephone lines, radio and television transmitters. When dispersed widely over a drainage basin, tephra can change rainfall/runoff relationships. Low permeability of fine ash deposits leads to increased runoff, accelerated erosion, stream-channel changes and hazardous floods. In contrast, thick, coarse-grained deposits closed to the source can increase infiltration capacity and essentially eliminate surface runoff.

Many of the hazards of tephra falls can be mitigated with proper planning and preparation. This includes clearing tephra from roofs as it accumulates, designing roofs with steep slopes, strengthening roofs and walls, designing filters for machinery, wearing respirators or wet clothes over the mouth and nose because tephra can contain harmful gases adsorbed on the particles as acid aerosols and salt particles.

Volcanic Gas

Magma is molten rock containing dissolved gases that are released to the atmosphere during an eruption and while the magma lies close to the surface from hydrothermal systems. The most abundant volcanic gas is water vapor; other important gases are carbon dioxide, carbon monoxide, sulfur oxides, hydrogen sulfide, chlorine, and fluorine. The gases are transported away from vents as acid aerosols, as compounds adsorbed on tephra and as microscopic salt particles. Sulfur compounds, chlorine and fluorine react with water to form poisonous acids damaging to the eyes, skin and repiratory systems of animals even in very small concentrations. The acids can destroy vegetation, fabrics and metals. Atmospheric veils of dust or acid aerosols caused by large-volume explosive eruptions can effect regional or global climate.

Most volcanic gases are noxious and smell bad, but they can cause mass fatalities. An rare case of mass deaths by volcanic gases in 1986 at Lake Nyos, in Cameroon, West Africa. Tons of carbon dioxide spilled out of Lake Nyos, and flowed silently down a canyon and through 3 village occupied by 1700 people. They and 3000 cattle died instantly from lack of oxygen.

Carbon dioxide emissions are now being monitored at Mammoth Mountain, California.


A tsunami is a long-period sea wave or wave train generated by a sudden displacement of water. Tsunamis travel at very high speeds through deep water as low broad waves and build to great heights as they approach the shallow bottom of shores. Most are caused by fault displacements on the sea floor, but many have been caused by volcanic action. The eruption of Krakatau in 1883 produced tsunamis that killed 36,000 people. The pyroclastic flow generated by this eruption displaced the water that initiated the tsunamis.

Copyright (C) 1997, by Richard V. Fisher. All rights reserved.

What causes a volcano to erupt and how do scientists predict eruptions?

When a part of the earth's upper mantle or lower crust melts, magma forms. A volcano is essentially an opening or a vent through which this magma and the dissolved gases it contains are discharged. Although there are several factors triggering a volcanic eruption, three predominate: the buoyancy of the magma, the pressure from the exsolved gases in the magma and the injection of a new batch of magma into an already filled magma chamber. What follows is a brief description of these processes.

As rock inside the earth melts, its mass remains the same while its volume increases--producing a melt that is less dense than the surrounding rock. This lighter magma then rises toward the surface by virtue of its buoyancy. If the density of the magma between the zone of its generation and the surface is less than that of the surrounding and overlying rocks, the magma reaches the surface and erupts.

Magmas of so-called andesitic and rhyolitic compositions also contain dissolved volatiles such as water, sulfur dioxide and carbon dioxide. Experiments have shown that the amount of a dissolved gas in magma (its solubility) at atmospheric pressure is zero, but rises with increasing pressure.

For example, in an andesitic magma saturated with water and six kilometers below the surface, about 5 percent of its weight is dissolved water. As this magma moves toward the surface, the solubility of the water in the magma decreases, and so the excess water separates from the magma in the form of bubbles. As the magma moves closer to the surface, more and more water exsolves from the magma, thereby increasing the gas/magma ratio in the conduit. When the volume of bubbles reaches about 75 percent, the magma disintegrates to pyroclasts (partially molten and solid fragments) and erupts explosively.

The third process that causes volcanic eruptions is an injection of new magma into a chamber that is already filled with magma of similar or different composition. This injection forces some of the magma in the chamber to move up in the conduit and erupt at the

Although volcanologists are well aware of these three processes, they cannot yet predict a volcanic eruption. But they have made significant advances in forecasting volcanic eruptions. Forecasting involves probable character and time of an eruption in a monitored volcano. The character of an eruption is based on the prehistoric and historic record of the volcano in question and its volcanic products. For example, a violently erupting volcano that has produced ash fall, ash flow and volcanic mudflows (or lahars) is likely to do the same in the future.

Determining the timing of an eruption in a monitored volcano depends on measuring a number of parameters, including, but not limited to, seismic activity at the volcano (especially depth and frequency of volcanic earthquakes), ground deformations (determined using a tiltmeter and/or GPS, and satellite interferometry), and gas emissions (sampling the amount of sulfur dioxide gas emitted by correlation spectrometer, or COSPEC). An excellent example of successful forecasting occurred in 1991. Volcanologists from the U.S. Geological Survey accurately predicted the June 15 eruption of the Pinatubo Volcano in the Philippines, allowing for the timely evacuation of the Clark Air Base and saving thousands of lives.


PDRRMO Office Location

Provincial Sports Complex, Brgy. Bolbok, Batangas City