2015

AZERBAIJAN

by RUSTAM SAFARALIYEVASIAN DISASTER REDUCTIONCENTER
1/1/2015

Disclaimer
This report was compiled by an ADRC visiting researcher (VR) from ADRC
member countries.
The views expressed in the report do not necessarily reflect the views of theADRC. The boundaries and names shown and the designations used on themaps in the report also do not imply official endorsement or acceptance by
the ADRC.

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ASIAN DISASTER REDUCTION CENTERAZERBAIJANCOUNTRY REPORT
by Rustam Safaraliyev

09/2/20153

Table of Contents
COUNTRY PROFILE....................................................................................................................................................... 5
GEOGRAPHY ..................................................................................................................................................................... 8
LANDSCAPE AND TOPOGRAPHY ........................................................................................................................................................ 8
CLIMATE ............................................................................................................................................................................................................ 9
MINERAL RESOURCES ............................................................................................................................................................................ 11
WATER RESOURCES ................................................................................................................................................................................ 12

CLIMAT CHANGES AND NATURAL HAZARDS .............................................................................................. 14
FLOODS AND LANDSLIDES .................................................................................................................................................................. 14
SEISMICITY ................................................................................................................................................................................................... 15
MUD VOLCANOS ......................................................................................................................................................................................... 18
FIRES ................................................................................................................................................................................................................ 19
UNDERGROUND WATERS ..................................................................................................................................................................... 19
HAIL .................................................................................................................................................................................................................. 19
STRONG WINDS.......................................................................................................................................................................................... 19
TEMPERATURE EXTREMUMS............................................................................................................................................................ 20
SURFACE FLUCTUATION OT THE CASPIAN SEA ...................................................................................................................... 20

RECENT DISASTERS .................................................................................................................................................. 21
FLOODS ........................................................................................................................................................................................................... 21
LANDSLIDES ................................................................................................................................................................................................. 22
MUD VOLCANO ERUPTIONS ............................................................................................................................................................... 23
EARTHQUAKES ........................................................................................................................................................................................... 23

EMERGENCY MANAGEMENT SYSTEM.............................................................................................................. 24
LEGAL BASIS................................................................................................................................................................................................. 24
OUTLINE OF THE MAIN ACTIVITIES.............................................................................................................................................. 24
ORGANIZATIONAL STRUCTURE OF THE MES .......................................................................................................................... 25

HYOGO FRAMEWORK FOR ACTION 2005-2015 ........................................................................................ 26
BIBLIOGRAPHY: .......................................................................................................................................................... 30

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COUNTRY PROFILEAZERBAIJAN – THE LAND OF FIRE. Azerbaijan is ageographical name. On the one hand this name islinked with the population, which lived in this region
for thousands of years before our era, and who were
mostly fire-worshippers. Local population consideredthat fire was their God and so they worshipped thefire. "Azer" means fire. The Turkic name "Azer" wasused for this territory for a long time. The word "Azer"
consists of two parts - "az" and "er" In Turkic
languages, "az" means a good intention and a fate ofsuccess. Thus, the word "Azer" means "a brave man","a brave boy", "the fire keeper".
Formal name: The Republic of Azerbaijan
The word "Azerbaijan" originatesfrom the name of an ancient
Turkish tribe, who resided in thoseterritories.
Location:

Azerbaijan is located between thecontinents of Europe and Asia in the southeast of the
Caucasus region and the western shores of the
Caspian between 38’24” and 41’54” latitude North,and between 50’51” 44’46” longitude.
Area: 86.6 thousand square km (forests 12%, waterbasins 1.7%, sown area 54.9%, including 31.1%
pastures and hayfields, 31.4% other lands).

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Bordering with:

Russia in the north – 289 km

Georgia in the north-west – 340 km

Armenia in the west – 766 km

Turkey in the west – 11 km

Iran in the south – 432 km

There is approximately 800 km of coastline along the
Caspian shore in the east.

Population: To July 2015, population of the Republic of Azerbaijan was estimated at
9,686,210. About 54.1 percent of population live in towns, while 45.9% in villages. Menconstitute 49% of population, while women 51%. Male–female ratio is 1000 to 1039.

Official language: Azerbaijani.
Azerbaijani language is the state official language of Azerbaijan and the mean of linguistic
communication of the 9 million population of the country.
Besides, Azerbaijani is also spoken by 20 million Azerbaijanis residing in the Islamic
Republic of Iran. Several millions of Azerbaijanis reside in Russia, USA, Turkey andWestern Europe. Regardless of their current country of residence, Azerbaijanis still canunderstand each other easily. There are over 30 million speakers of Azerbaijani at present.
6Genealogically, Azerbaijani language belongs to the Turkic group of languages and,
together with closely associated Turkish, Turkmen and Gagauz languages, forms thesouthwestern group of Turkic languages.

Capital City – Baku.
Baku is the capital of the Republic of Azerbaijan. It is a large scientific, cultural andindustrial center. Ancient foundations, a large area and population all make Baku one of theoldest and largest cities in the East.
Baku is situated on the shore of the Caspian Sea in the south of the Absheron
peninsula. It covers an area of 2,200 square km and has a population of 2 million. Nearly
500,000 refugees from Armenia as well as IDPs from the occupied territories, currently
reside in Baku.
People have lived and founded their settlements in Baku city and the Absheron
peninsula since ancient times. This was motivated by continuous migrations from north tosouth and from west to east due to the physical and geographical conditions, a favorable
location in the center of trade routes that crossed Silk Road, climatic conditions, productionof petroleum fuel in ancient times and the availability of large power resources.
Baku was one of the main cities in the Shirvanshakhs State in the 12th century, in the
Sefevids State in the 14th century, in the Ottoman Empire in the 16th century, and became
the capital of the Baku khanate in the 17th century.
Baku has 11 administrative districts and 5 settlements.

Silk Road

Baku Boulevard

7Religion: Islam (93%), other religious minorities: Judaism, Christianity, Albanian-Udi Church
Currency: Manat
International dialling code: +994
Internet domain: .az

GEOGRAPHYLANDSCAPE AND TOPOGRAPHYThe Republic of Azerbaijan is situated in the Alp-Himalayan mountain belt. The threemountain ranges are the Greater and Lesser Caucasus, and the Talysh Mountains, together
covering approximately 40% of the country. The highest point in the country is on Mount
Bazarduzu (4,485 m above sea level) situated in the Greater Caucasus. Lowlands and plains
make up the other 60% of the country. The average height of the country is 657 m above sea level,
however 18% of the country is below sea level. Azerbaijan is located in an active seismic zone,
with particularly high activity in the southern part of the Greater Caucasus, the Ganja region in theLesser Caucasus, and in the Autonomous Republic of Nachichevan. Azerbaijan does not extend
over a large geographical area, and much of the differentiation of landscapes is due to thevariation of altitude. Landscapes are influenced by climate, soil, and habitats that change withincreasing altitude. Landscapes replace each other with height, graduating from lowland plains,semi desert, steppe, forest, alpine meadow to subnival communities at the greatest heights of themountains, creating landscape zones at different altitudes. This altitudinal zonation is naturally
disordered in the Lankoran region as a result of the Talysh mountains where semi arid landscapes
replace the forest landscapes normal in the mountains. In Nakhichevan, forests develop in islands
due to local climatic conditions. The highest point in Nakhichevan Autonomous Republic is Gapijig
mountain (3,906 m). Other important mountain ranges include the Zangazur and Daralayaz
ranges in the northeast of the region, where there are a number of peaks over 3,000 m. A third of
the territory of Nakhichevan is covered by grassland/steppe, totaling some 172 km2, of whichsome 10,000 ha is salinated.

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Topography map of Azerbaijan

CLIMATE
Azerbaijan is a country of varied climates, although it is predominately subtropical. On
average, there are 1900-2900 hours of sunshine annually (approximately 5-8 hours dailysunshine). In the lowlands, summers are hot, and winters are moderate, however in the mountains,
the summers are cooler, and temperatures in the mountains can reach negative figures.
Humidity tends to be low, although it varies across the country.
Annual average temperature: +14.5oC
January: +1.7oC
July: +27.9oC
Max to +44o (Julfa, Nakhchevan)
Min to-42o (Great Caucasus Mountains)
Annual average number of precipitation: 500 mm (min 200, max 2300)

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Climate Map of Azerbaijan

Taking into consideration distribution and features of regime of weather temperature andatmosphere precipitations, as well as humidity circumstance in Azerbaijan Republic, 9 of 11
climate patterns of the Earth (according to V.V.Keppen) are determined here. Many of thesepatterns are divided into semi-types.

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MINERAL RESOURCES
Azerbaijan has rich natural resources. Main natural resources are oil and natural gas.
Famous oil and gas fields are in Absheron Peninsula and Caspian shelf.
Fields in Siyazan region north to Absheron peninsula have good potential. There are oilfields towest and south-west of Absheron in Gobustan, Shyrvan, Salyan plains. At present big oil fields
were discovered in water area south to Absheron. Gas fields are also very important. There isunique therapeutic oil type (Naftalan) discovered in Ganja city.
Azerbaijan has rich resources of iron ore and alunite. There are reserves of sulphurous pyrites,
molybdenum and arsenic. Polymetallic ore fields in Filizchay in the upper flow of the Balakan River
have industrial importance.
Main iron ore fields are in Small Caucasus Mountains (in Dashkasan). In north hills of Small
Caucasus Mountains there is alunite field in Zailyk region and this field is one of the biggest alunite
fields in the world. Also there are cobalt and sulphurous pyrites reserves near these regions(Dashkasan-Ganja regions). Gadabay, Tovuz, Ordubad, Kalbajar and Zangilan regions have richgold, silver and copper reserves. Rock-salt (Nehram field has reserves of 2-2.5 billion tons),
arsenic and molybdenum (in Paragachai) fields are being developed in Nakchyvan.
Azerbaijan soil has large reserves of various construction materials. Marble, which is not different
from “karrar” marble, also beautiful and strong tuff is extracted within the territory of Small
Caucasus Mountains. In Absheron peninsula gravel, sand, lime, fire resistant and brick clay is
being produced. The Republic has resources of 300 billion tons of building stone (Guzdak,
Mardakan, Dovlatyarli, Dilagard, Shakhbulag, Naftalan and Dash Salakhly) and 24 million tons offacing material (Gulbakht, Dashkasan, Shaktakhty, Gulably).
Azerbaijan has more than 1000 cold, mineral and thermal water resources. Most famous of theseresources are Istisu, Turshsu, Badamly, Galalty, Shikhburnu, Surakhany.

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Mineral resources of Azerbaijan

WATER RESOURCES
The main sources of water in Azerbaijan are the surface waters. However, only 24 of the
8350 rivers are greater than 100 km in length. All the rivers drain into the Caspian in the east of thecountry, through three main river basins - the Caspian Basin, (rivers draining directly into the
Caspian), the Kura basin (in western and central Azerbaijan) and the Araz basin.
The average density of river networks is 0.39 km per km2, with most of the rivers occurring in theKura basin.
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Of the 300 natural lakes in Azerbaijan, only six cover more than 10km2 of land area. The total areaof these six lakes makes up 83 % (250 km2) of the total lake area. The lakes of the Kura and Arazbasins (in the lowlands) are affected by upstream water management, causing an increase insalinity (5000-13000 mg/L), and a reduction in fish populations. Lakes on the Absheron Peninsula(on the shores of the Caspian) have become salinated as a result of upstream management andpolluted by industrial and domestic waste (especially from oil fields). In addition, the number andsize of lakes in this area are being artificially increased.
Lakes in the mountainous area tend to be small (the total area of the 90 mountain lakes is 2 km2),
but face few anthropogenic threats, because of their distance from settlements and industry.
In the last 40-50 years many water reservoirs have increased five-fold, so that they now cover
1070 km2. Total volume of these artificial lakes is 22.66 km3, but only 11.24 km3 is usable water.
The biggest of these by far is Mingachevir Reservoir, located along the River Kura which has atotal volume of 16 km3 and covers some 625km2. The water in reservoirs is used primarily forelectricity production and irrigation purposes. A dense network of channels irrigates more than
1300 ha of drought prone land. The channels also carry clean water to a number of settlements,
although approximately 40% of fresh water in Azerbaijan is taken from subsoil reserves.

Rivers, Channels, Collectors/Drains

13CLIMATE CHANGES AND NATURAL HAZARDSClimate change is an ecological problem on a global scale that poses a recognized threat
to all ecosystems and associated biodiversity. Predictions suggest that climate change is likely tohave a negative impact on ecosystems in Azerbaijan and may result in increased flooding anddesertification, fragmentation of habitats, and species extinction. Over the last century the airtemperature in Azerbaijan has increased on average by around half a degree Celsius, with thehighest changes in temperature recorded from the Greater Caucasus and the Kura-Araz lowland(0.5 - 0.6oC) and lowest changes recorded in Minor Caucasus and along Caspian shoreline.
Based on global models of climate change, experts estimate that average temperatures in
Azerbaijan could increase by as much as 2oC. Associated with this it is expected the incidence oftemperature extremes will increase, as will extreme weather events. Particularly important, is apredicted decrease in humidity for much of Azerbaijan.
Such increases could affect the availability of water (particularly in arid regions), which could inturn impact on irrigation, drinking water, and power production. Biological systems would also beaffected under this scenario, with predictions of changed ecosystem dynamics and degradation offorest zones. The predictions suggest that the area of deciduous forest will decrease by 20%,
while coniferous woodland will increase by 12%, and scrub coverage could increase by as muchas 70%. The area of oak forest could reduce by 2-3%, although areas of beech would increase by
15% and hornbeam by 19%.
The warmer climate could increase productivity for a number of plants, and this would favour
increased agriculture (including vineyards, cotton and fodder production). However, the increasein evapo-transpiration from the soil could result in increased salination and erosion, ultimately
leading to desertification.

FLOODS AND LANDSLIDESTerritory of Azerbaijan Republic is included in the list of areas, where floods andinundations are observed mostly along the world. Appearance of floods in Great and Little
Caucasus mountain ranges which cover almost half of countrywide territory, occurs more
intensively. Most floods and inundations happen in uplands of South slope of Great Caucasus
and Nakhichevan AR. The expected climate changes can cause serious difficulties in the
future by increasing recurrence of floods and overflows.

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Heavy showers on the territory of Azerbaijan Republic often lead to floods with damages andhuman casualties. Moreover, hail fall is observed on the territory during warm periods. They cause
damage to agriculture. Hail diameters sometimes are about 30–50 millimeters, which results intotal destruction. A substantial part of central Azerbaijan could be flooded in case of damage to the
Mingechevir water reservoir in the west.
Landslides caused by heavy rains and underground water are also common case for Azerbaijan.
Besides, another reason of landslides in rural regions of Azerbaijan is semi-nomadic animalhusbandry. As a result of increasing livestock in the country on the semi-nomadic principle, theland is subjected to erosion, resulting in landslides.

SEISMICITY
As a part of the Alpine folded system Azerbaijan territory characterized as very highseismic activity. Strong and catastrophic earthquakes which happened several times in this areafrom ancient times till now caused large number of human loses and destructions.
The strongest earthquakes mainly have been registered in Shamakhi and Ganja regions. The
earthquake happened in Shamakhi in 1668 (M ≈ 7.0; İ0 = 9-10 points) 2 can be considered as oneof the strongest earthquakes happened in the Caucasus up to now.

427--1930.
Epicenters map of earthquakes (M≥5,0) happened in Azerbaijan territory in 427

15

According to historical information this earthquake resulted with landslides and more than 80,000
people died.
In Shamakhi region registered seismic shocks with intensity up to 8 according MSK-64 in 1828,
1859, 1869 and 1872 years. In this area the last catastrophic earthquake (M = 6.9; İ0 = 9 points)
happened in 1902.
Other area where happened destructive earthquakes is Ganja region. In this area happened
strong earthquakes in 427 (M ≈ 6.7; İ0 = 9 points), in 1139 (M ≈ 6.8; İ0 = 9 points), in 1235 (M ≈5.7; İ0 = 8 points). After earthquake happened in 1139 because of landslide created Goy-gol Lake.
In another regions of republic also were registered a number of strong earthquakes. Intensity ofthese earthquakes was not more than İ0= 6-7 points, but in many cases resulted with many
destructions.
Since 2003 in the Azerbaijan territory installed 30 telemetry seismic stations production of“Kinemetrics”. Up to now in republican territory working analogue seismic stations also. During
installation of these stations it was taking into account the level of the seismicity of selected
territory.
Last years seismic stations with higher sensitivity seismographs has been added to the
Republican Seismic Stations Network and after this it become possible to register even lower
intensity (magnitude) earthquakes in republican territory.

The map of Kinemetrics Seismic Stations

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Seismic Zonation Map of Azerbaijan

Active tectonic faults in the terrirotory of Azerbaijan

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MUD VOLCANOS
Mud volcanoes are pervasive within the Republic of Azerbaijan. There are over 220 mud
volcanoes in Azerbaijan (Absheron Peninsula, Gobustan, southeast Shirvan plain, Samur-Davachi
plain terrane, both Absheron and Baku Archipelago. The biggest are Galmas, Toragay, Big
Kanizadag etc. Most of them have a cone shape. Their height varies in the range from 20 to 400m,
whereas base diameter may vary from 100 to 4500m.
Besides onshore mud volcanoes there are buried volcanoes and offshore mud volcanoes. There
are over 140 offshore mud volcanoes within the Caspian Sea. Eight Islands within Bakuarchipelago were generated by mud volcanoes eruptions (Khara-Zira, Zanbil, Garasu, Gil,
Sangi-Mughan, Chigmil etc).
Mud volcanoes are one of the visible signs of the presence of oil and gas reserves under the landand sea in the Caspian region. Gas seeps are a related phenomenon. These occur when a pocketof gas under the ground finds a passage to the surface. These occur when a pocket of gas under
the ground finds a passage to the surface. One gas seep burns continually on a hillside near Baku,
ignored by the sheep but sometimes visited by curious tourists.
It is an unearthly sight, especially at dusk, and it is easy to understand how these fires that neverappear to burn out became objects of worship.
The appearance of the Zoroastrian religion in Azerbaijan almost 2,000 years ago is closely
connected with these geological phenomena, and, according to one theory, the name "Azerbaijan"
itself was derived from the word for "fire" in Persian.
Geologists agree on some aspects of the formation and activities of mud volcanoes. They areformed when mud and sand up to several kilometres beneath the Earth's surface are squeezed
upwards by compressive forces and expelled.
The origins of the volcanoes are disputed. Mud volcanoes are often formed in areas of weakness
in the Earth's crust, along fault lines, and are associated with geologically young sedimentarydeposits, the presence of organic gas from hydrocarbon deposits, and overlying pressure which
forces this gas to the surface.
But when it comes to accounting for the differences between mud volcanoes, their varying shapes
and sizes, the gases they emit and their unpredictable behaviour, there is little agreement.
Geologists describe mud volcanoes as "capricious", and are still arguing about exactly how they
are formed. Some believe they are created during the sedimentary process itself, while othersargue that different processes are also involved, for example, seismic activity.
To the non-geologist, the explanations can seem, well, as clear as mud. But the arguments about
their origins only add to the aura of mystery that surrounds these unusual and enigmatic
phenomena.
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FIRES
Deciduous/leaf bearing forests dominate mainly in Azerbaijan, therefore forest fires are
not specific for the republic. But fires happened as a result of anthropogenous impacts can cause
to extinction of various species of flora and fauna. Majority of fires occur due to burning of fields
after corn reaping mainly in arid cycle. So that 7 forest fires happened in 2002 covered 46 ha area.
But fire-fanging of hay, then trees appears in spring-summer seasons in Talish ranges. Six forest
fires happened in 2007 covered 88.3 ha area, four forest fires in 2008 covered 25.3 ha area.

UNDERGROUND WATERS
Underground waters constitute 24 million m3 in a day (8.8 km3 in a year) being formed infoothills of Great and Little Caucasus and plain areas, Nakhichevan and Talish ranges of thecountry. Presently, 5 million m3 or only 20% of overall resources are used in a day. It shows
possibility of widely usability of underground water potential of the country in water deficiency
period.

HAIL
Most recurrence of hail precipitations is observed in uplands and foothills of Great andLittle Caucasus. Agriculture plants mostly suffer from frequent hail-hits.

STRONG WINDS
Orographic features of the area enable west winds to become stronger along Kura river
basin and west coasts of the Caspian sea as well as east winds in the territory of Nakhichevan AR.
An increase tendency of number of very strong windy days (more than 25 m/second) is observedin the republic within the last years according to statistic analyses carried out. So that within
2002-2008 maximum speed of wind in territory of the republic reached to 38-40 m/second in Baku
and Absheron cities, Ganja-Shamakhy-Zardab-Zagatala regions (Alibay) in August 2005, in March
2006 and February, March, August, September 2007.

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TEMPERATURE EXTREMUMS
Temperature stresses adversely effects wildlife and vegetation. Exceedence of absolute
maximums and minimums of air temperature were observed within past 15 years in the lastcentury. Declining of minimum temperature in a considerable extent in winter led to damages for
subtropic plants. Within 2002-2008 maximum air temperature in territory of the republic totalled to40-430 hot (July 2005, August 2007) in some Central Lowland regions, minimal temperatureequalled to 14-170 frost (February 2005, March 2006) in uplands. Minimum air temperature in
Baku and Absheron peninsula was observed as 8.70 frost in January 2008 that it is a record.

SURFACE FLUCTUATION OT THE CASPIAN SEA
Beginning from 1978 up to 1995 485 km2 coast line of Azerbaijan remained under waterat the result of the growth of sea level 2.5 m in the Caspian Sea. At the result of the growth of thelevel in the Caspian Sea the sea is re-polluted with the oil products. Biogenic elements, organic
substance, and heavy metals amounts increase at the result of washing the areas under water orwater pressure. Also there were changes in the estuary of the Kura; so in comparison with 1979
the thickness of the sludge grew 1.2-1.4 m. According to the modern research results highhumidity will be kept in the Caspian Sea basin as the result of climate heating. If the level grows
150 centimeter, in the Caspian Sea 87,7 thousand ha will remain under water and it will occupy20

1,6% of Azerbaijan area. At the result of expected growth at the Caspian Sea level is one of theimportant factors to influence the multiply of mine fish. The multiply of mine fish in the river will
decrease; the quality of the water on the coastline will deteriorate and the places for spawning will
get to worth in shallow coastal areas because of the growth in the sea level.
Surface level of the sea equalled to -27,12 m Bsn in 2008. Surface level of the Caspian sea wasremembered with large fluctuations within the history. Surface level fluctuations cause greatdamages to the economy of Azerbaijan Republic. According to opinions of some specialists,surface level of the Caspian can rise up as 1.2 m until 2020.

RECENT DISASTERS
FLOODS
There observed heavy floods and overflows in the rivers refulted from snowmelt onmountainous areas and showery rains because of a sharp rise in temperatures over mountainy
areas of Great and Little Caucasus within 2003-2008.

1.

Due to shower rains (Guba 33mm, Khachmaz 23mm, Rustov 59mm, Gusar 38mm,
Tangaalty 20mm, Kupchal 16mm) on July 8, 2008 , floods and overflows passed through the rivers

21

of Gusar, Gudiyal, Valvala, Guru, Jaghajug, Gilgil. Level of water surface rised to 2 m. As a result,level meter units underwent to flooding, hydraulic works were damaged and some habitats,electric piles, roads and bridges suffered considerably, finally 1 person died in overflow. Due toshower rains (Dashkasan 24mm and Goygol 22mm) on July 8-9, floods and overflows passed
through the rivers of Goshgar, Kurak, Dastafyurd and Ganja. As a result, level meter units
underwent to flooding, hydraulic works were damaged, arable lands were out of use, telephoneand electric piles were broken down, private cars turned over, roadways suffered and 1 military
serviceman died in overflow while passing across the river. Level of water surface rised as 157 cm
in Lankaran river, 105 cm in Sefidor river and 117 cm in Vasharu river due to shower rains(Dashdatuk 49.8 mm and Lankaran 25.6 mm) on October 2-3 (in the evening and at night). Thereemerged short-term floods in Pensar river flowing across territory of Astara region andsubsequently 2 persons, i.e. mother and her child remained under floods while passing throughfootbridge. Horned livestock and bridges underwent to flooding in some villages.
(www.cbd.int/doc/world/az/az-nr-04-en.doc)
In May 2010 unusually large amounts of rain in Southern Azerbaijan caused the Kura River to rise
to its highest level in over 100 years, bursting dams and overflowing onto nearby villages. This
unprecedented level of flooding hit hardest in the Sabirabad, Imishli, Saatli districts, which is near
the confluence of the Kura and Araz rivers. More than 24,000 people were affected with tens of
thousands of homes flooded or destroyed and 50,000 hectares of farmland inundated.

2010 flooding area

LANDSLIDES
On 7 March 2000, a major landslide involving an area of 15 ha occurred in the Bayil zoneof the Sabayil district, south of Baku city center. The landslide in the Bayil slope destroyed dozens

22

of shops, apartments and gas stations. After the incident, it was decided to move roughly 300
families from this territory. A total of 140 families were moved by 2003. The slope in later years
also experienced few minor landslides which led Baku City Administration to examine the area andmake a final decision on razing houses in this territory.
Analysis of the landslide mechanism and its causes revealed that it was a single compound slidewith one slip surface, which was triggered by intense rainfall during October and November 1999
(more than the average annual precipitation occurred within two months).
Due to the low permeability of the soil, the groundwater table was slowly recharged; but theinvestigations after the disaster showed that the crack openings in the landslide zone had allowed
a significant lowering of the water table. Some water leakage from utility lines crossing the slide
may also have had a detrimental preparatory effect.

MUD VOLCANO ERUPTIONSAn impressive volcanic eruption occurred in 2001 in Azerbaijan, but there were nocasualties or evacuation warnings. The biggest flames burned for about five minutes. Then there
was another huge explosion, and then they calmed down to about 10 or 20 metres (32 or 65 feet)high. The flames could easily be seen from 15 kilometres away on the day of the explosion, andwere still burning, although at a lower level, three days later.

Shikhzayirli mud volcano erupted in Gobustan region of Azerbaijan on March 13, 2011.Witnesses
heard explosions before the eruption, mud breccia erupted and then fire blazed up in the territoryof the volcano.The fire had an altitude above 50 m. Experts and rescuers of the Ministry of
Emergency Situations immediately arrived at the site to prevent any emergency situation. After its
activation decreased and mud flows were seen in some bald peaks. Deep grikes were createdaround the crater. The mud volcano didn't threaten the nearby villages.

EARTHQUAKES
The 2000 Baku earthquake occurred on Saturday, November 25, 2000 at 22:10 (18:10
GMT) local time, measuring 7.0 on the Richter scale in the epicentre with 6.3 in Baku, Azerbaijan,
and three minutes later followed by a quake measuring 5.9. No human loss or material damage
23

was registered.

EMERGENCY MANAGEMENT SYSTEMLEGAL BASIS
Established by the Decree of the President of the Republic of Azerbaijan, in 16 December
2005, Ministry of Emergency Situations of the Republic of Azerbaijan is the central executive bodyof the government, which is responsible for emergency management within the entire territory of
the country. According to the decree “for the purpose of providing prevention of natural andman-made disasters and fires, elimination of their consequences, management of activities of therelevant bodies responsible for rescue and rehabilitation works by one centralized system,
organization and realization of civil defense work in the country, the Ministry of Emergency
Situations of the Republic of Azerbaijan is established.”

OUTLINE OF THE MAIN ACTIVITIES Protection of population and territories from fires and disasters; Prevention of emergency situations and elimination of their consequences; Ensuring of safety rules water basins, building sites, industrial and mining enterprises andsafe movement of small ships in state waters
 Establishment and proper management of the State Resource Fund; Organization of protection of strategic objects exposed to natural, man-made and terror
threats, neutralization of radioactive wastes; Organization of quick response to emergency situations and management of humanitarianaids;
 Organization of management rescue-searching and first aid, aviation and other transport
life-saving operations in case of emergency
 Organization of awareness-raising activities among population regarding life safety rules
and measures, methodical guidance over respective work done in this field by state bodies
and public organizations etc.

24

ORGANIZATIONAL STRUCTURE OF THE MES

25

HYOGO FRAMEWORK FOR ACTION 2005-2015
As a signatory of Hyogo Framework for Action 2005-2015 Azerbaijan undertook several
responsibilities. Since then, which coincides with the establishment year of the Ministry of
Emergency Situations set of measures towards reaching goals laid down by the Hyogo
Framework for Action 2005-2015 has been taken and action report is to be prepared by the end of
this year.
In this connection, in April 2011, UNICEF, in partnership with the Government of Azerbaijan,
organised a one day seminar in Baku to discuss national efforts to ensure safety and protection ofchildren against future disasters. This “Hyogo Framework for Action and Disaster Risk Reductionin Education” seminar brought together government officials from different ministries, and staff
from the UN, national and international NGOs to discuss the Hyogo Framework for Action. The
group also discussed the country’s progress so far and way forward for Disaster Risk Reduction(DRR) in Education in Azerbaijan. The seminar was organized in collaboration with the Ministry of
Education and the Ministry of Emergency Situations under their project “Supporting Disaster Risk
Reduction amongst Vulnerable Communities and Institutions in Azerbaijan”. As it was said byAsim Rehman, UNICEF Regional emergency specialist, “The number of participants
demonstrated how important DRR is for the country, and the seminar was planned to be a usefulmechanism for sharing of information and experience on school safety assessment tools andcurriculum integration from pre-school to secondary”
The next conference related to Hyogo Framework commitments of the country is planned to beheld in November 15, 2011, Baku, Azerbaijan by the Association of Civil Protection and Life Safety
Specialists “Fovgal”, Azerbaijan Architecture and Construction University, Baku office of theEuropean Center on Training and Information of Local and Regional Authorities and Population in
the Field of Natural and Technological Disasters.

Several ministries and other relevant

government bodies is invited to the conference on “The role of the local authorities andmunicipalities in providing protection of population, economy and environment according toCommunities- Hyogo Framework for Action 2005-2015”.

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Progress on the Implementation of Hyogo Framework for Action andforthcoming Major Projects on Disaster Risk Reduction

UNICEF, in partnership with the Government of Azerbaijan, organized seminar in Baku to
discuss national efforts to ensure safety and protection of children against future disasters. This
“Hyogo Framework for Action and Disaster Risk Reduction in Education” seminar brought together
government officials from different ministries, and staff from the UN, national and internationalNGOs to discuss the Hyogo Framework for Action - which was endorsed by 168 governments inJanuary 2005 and is the global blueprint for disaster risk reduction. The group also discussed thecountry’s progress so far and way forward for Disaster Risk Reduction (DRR) in Education in
Azerbaijan.
The seminar was organized in collaboration with the Ministry of Education and theMinistry of Emergency Situations under their project “Supporting Disaster Risk Reduction amongst
Vulnerable Communities and Institutions in Azerbaijan”. This EU-funded initiative emphasizes theneed for a systematic approach to disaster risk reduction and advocates for mainstreaming achild-focused DRR policy and strategic framework into existing policies, planning and programs foreducation or in some other way related to disaster preparedness.
UNICEF will continue preparing children and vulnerable communities to respond to futuredisasters, and that everyone present will be active in advocating for and implementing measuresthat will help reduce the disastrous consequences of natural hazards on children and women in
Azerbaijan. The seminar should also lay an important foundation for improving existing27

governmental strategies and documents on disaster risk reduction in Azerbaijan with a particularfocus on education,” he said.
UNICEF’s approach to DRR in education is at two levels - policy level dialogue on
curriculum and disaster management, coupled with school based interventions reaching, inparticular, teachers and schoolchildren. Children are important first because they are the mostvulnerable in a disaster, but also because they possess unique abilities to contribute to thecreation of a culture of safety and prevention.
Concluding remarks of the seminar included:
It is important to spread information and knowledge on the Hyogo Framework and DRR
in education at national and local levels. The idea of having similar events at
district level was suggested by UNICEF.
DRR is everybody’s responsibility. All line ministries implementing state programs andwork plans should integrate DRR into their planning. Inclusion of children with disabilities into allschool-based activities and improving early warning and detection in the area of flooding areimportant.
The key to success in implementing the HFA and indeed any DRR intervention iscoordination between all respective parties and ministries not just in education. By starting and insome cases maintaining co-operation between all key stakeholders and if possible using existingco-ordination mechanisms, the issue will be remain a high priority.
Whilst what UN is currently doing is a pilot project, it provides a good opportunity to learn
lessons and good practices which can be used in the future for Azerbaijan and in other countries.

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A conference held on 10th August 2010 to sum up the “Supporting Disaster Risk
Reduction

amongstVulnerable

Communities

andInstitutions

in

Azerbaijan”

project

co-implemented by the UNICEF, Ministries of Education and Emergency Situations. The project ispart of the Disaster Risk Reduction in education program financed by the DIPECHO, the Disaster
preparedness branch of the European Commission’s Humanitarian Aid Department.
UNICEF Deputy Representative in Azerbaijan Rashed Mustafa told of the aims of the project
realized since 2010. Speaking at the meeting, UNICEF Coordinator for DIPECHO Aisloing
Falconer pointed out disaster response monitoring had been carried out in 10 pilot schools in six
regions of Azerbaijan over preparation and emphasized the importance of disaster response
education at schools.
The conference discussed mechanisms of national coordination for disaster risk
education in education and future projects.

29Sub-Regional Office of the United Nations International Strategy for Disaster Reduction(UNISDR) for Central Asia and the Caucasus and the Ministry of Emergency Situations of the
Republic of Azerbaijan, with support from UNDP, hold a workshop on National Platform forDisaster Risk Reduction on 20 October 2010 in Baku.
The workshop will brought together representatives of the relevant Government ministries
including the Ministry of Emergency Situations, Ministry of Ecology and Natural Resources,
Ministry of Health and Ministry of Industry and Energy, bilateral donors, international and nationalNGOs and media. Ms. Goulsara Pulatova, Regional Coordinator of UNISDR Central Asia &Caucasus office and Mr. Abdurahim Muhidov, HFA Coordinator facilitated the Workshop.
The overall purpose of the meeting was to bring together all stakeholders in the area of
disaster risk reduction (DRR) and potential partners of the National Platform to discuss ways toimproving national coordination in disaster risk management and risk reduction, as well asreporting on the progress achieved in the country. The UNISDR officers will make presentations on
UNISDR, the activities in the region of Central Asia and Caucasus, the Hyogo Framework for
Action, the structure and the contents of the national report on HFA.
The country reports are used in compilation of the regional progress reports, and in the
Global Assessment Report which is published every two years, at the Global Platform for Disaster
Risk Reduction. The sessions of the Global Platform were held in 2007 and 2009, and the next
one is planned for May of 2011 in Geneva.
The idea of the workshop was first discussed and agreed with the Government of
Azerbaijan in December 2009 when UNISDIR sent a mission to Baku to introduce its mandate to
the Government and establish contacts with the relevant governmental and non-governmentalorganizations, UN agencies and international NGOs working in the country.

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As part of the development of a post-2015 framework for disaster risk reduction, thesecond regional consultation meeting for the Central Asia and South Caucasus countries met in
Almaty, Kazakhstan on 1-2 April 2014.
The Governments of Armenia, Azerbaijan, Georgia, Kazakhstan, Kyrgyzstan, Tajikistan
and Uzbekistan attended along with disaster risk reduction experts from other stakeholders
including international organizations, donors, UN Resident Coordinators, NGOs and civil society.
More than 160 representatives attended the consultation. UNISDR and the Government of
Kazakhstan co-hosted the consultation. Central Asia and South Caucasus countries experience
many hazards and are particularly susceptible to floods and earthquakes. Over a 30-year period
from 1980, 14 million people were hit by 131 major disaster events with economic losses of an
estimated USD3.8 billion.
The major hazards are of regional character, which requires strengthening cross-bordercoordination and exchange of information on sub-regional and regional level. The countries share
the need in education, training, technologies and methodologies in risk and loss assessment,
inclusion of all sectors and all population groups and sectors of economy in disaster risk reduction,
as well as their protection and building their resilience. Addressing these and other needs andgaps is crucial for ensuring sustainable development of the region and of each of the countries.
A post-2015 framework for disaster risk reduction to be considered at the 3 rd UN World
Conference on Disaster Risk Reduction in Sendai, Japan on 14-18 March 2015 will help to refocus
regional efforts and provide guidance, actions and commitments to reduce risks and build
resilience. The consultations for the countries in the Central Asia and South Caucasus region
reflected on the existing Hyogo Framework of Action and developed recommendations forconsideration as well as volunteer commitments to assist in the implementation of a post-2015
framework for disaster risk reduction. The two day consultation included one day of thematic andstakeholder consultations that have been prioritized over the last few years in Central Asia andSouth Caucasus countries including: local governments; risk information; education and training;
NGOs and civil society; gender; safe schools and hospitals; regional cooperation; water-related
disaster cooperation. The second day focused on statements and commitments from
Governments, the thematic groups and the stakeholders.
Within the two days of consultations a number of results and some overarchingmessages; ten general recommendations for a post-2015 framework for disaster risk reduction;
and a number of specific recommendations on thematic and cross-cutting areas were developed.
The recommendations reflect the current priorities of the Central Asia and South Caucasus
countries on reducing the risk of disasters and protecting their populations.
A. Overarching Messages
Future generations must have a safer and resilient planet. Disaster risk reduction is31

development that builds a safer and more resilient planet. The integration of disaster risk reduction
into the post-2015 development agenda and climate agreements is therefore fundamental for asustainable future.
B. General Recommendations
1. Develop long term disaster risk reduction and climate adaptation programs at national
and local level. Ensure inclusion of disaster risk reduction approach to overall development
programs and plans.
2. Local level risk management and development of resilient cities should be linked toand harmonized with the national development plans.
3. Risk assessment and the governing of risk should be integral to development planning.
4. Formulate and implement national level policy on disaster risk reduction.
5. Ensure greater coordination of roles and efforts between ministries of emergency
situations with other ministries, public authorities, private sector and NGOs at the national andlocal level.
6. Ensure connection between national level planning, monitoring and review and a
post-2015 framework for disaster risk reduction and other relevant international agreements.
7. Further improve and strengthen policies, legal regulations and law in disaster risk
reduction.
8. Disseminate knowledge and experience on disaster risk reduction gained from HFA
implementation.
9. Engage stakeholders and make special efforts to include media, the business sector
and vulnerable families and groups in disaster risk management planning and partnerships.
10. Recognize that recovery is an opportunity to build back better and reduce thevulnerabilities of countries. An internationally agreed framework for cooperation that covers
recovery will be useful in assisting disaster-affected nations both in guidance and to help build
more capacity
C. Specific Recommendations
The thematic and stakeholder groups’ consultations also provided a number of specificrecommendations for consideration for a post-2015 framework for disaster risk reduction. They
reflect the work and priorities of disaster risk reduction in Central Asia and South Caucasus. In theSummary Report, these have been grouped on the specific themes of: information and risk
assessment; education and training; safe schools and hospitals. Then there were also a set ofcross-cutting recommendations which were evident in many of the consultation reports andstatements including around: capacity building; inclusiveness; gender and the role of women;measures for success and accountability (monitoring and indicators); and, regional cooperation.

32

(i) Information and risk assessment• Provide access to timely, reliable and objective information on risks and hazards aheadof disasters, as well as life-saving information during and after disasters.
• Take measures for targeted development of coordinated methods/approaches on risk
assessment and simulation, application of remote monitoring methods and disasters forecasts,
damage and loss analysis with the aim of effective disasters risk management.
• Create specialized programs for risk assessment and information management.
• Promote and ensure collection, analysis and dissemination of sex and age
disaggregated data on disaster risks, occurrence, impact and losses at all levels (including in linewith the new indicator system on disaster risk reduction).
• Risk and vulnerability assessments to be gender-based and include gender-analysis.
• Use modern technologies for hazard monitoring and early warning of population.
• Provide technical and financial support from the specialized agencies of the United
Nations and from the developed countries in the field of remote sensing.
• Establish platforms for information generation and exchange between countries of theCentral Asia and South Caucasus region. Promote and build partnership with academia andresearch institutions, to generate solid evidence on climate change and potential disasters andtheir socio-economic impact.

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BIBLIOGRAPHY: Official wep-page of the Ministry of Emergency Situations of the Republic of Azerbaijan.
Available at: www.fhn.gov.az
 Official web-page of Ministry of Ecology and Natural Resources of the Republic ofAzerbaijan.
Available at: www.eco.gov.az/en
 www.azerbaijan.az
 Official web-page of the Republican Seismic Survey Center
Available at: www.seismology.az
 Official web-page of the Fund of Monitoring of Ecological Standards of Azerbaijan
Available at: www.azecology.az
 Country Study on Biodiversity of Azerbaijan Republic. Fourth National Report toConvention of Biological Diversity.
Available at: www.cbd.int/doc/world/az/az-nr-04-en.docSimilar
 NATO Seismic Hazard Assessment for Azerbaijan
Available at: http://presentations.copernicus.org/EGU2011-2738_presentation.pdf

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