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E

conomic

D

evelopment

and

W

ater

west side to 20

o

C in the south of the island. Precipitation

patterns are highly varied, with mean precipitation

ranging from 327 mm in coastal areas to 2,161 mm in the

headwaters of the White mountains.

6

The highest precip-

itation is observed in the mountains, with much less on

the north coast of the Chania prefecture and south part

of Irakleion. During recent decades a decreasing trend in

annual precipitation has been observed, with the largest

reductions in higher elevations.

7

The combination of the Cretan mountainous relief,

complex geology, long coastline and the remoteness

of some biotopes has led to great diversity and the

existence of many endemic and rare animal and plant

species. The national Woodland of Samaria (4,850 ha)

has been categorized as a Biosphere Reserve by the

United Nations Educational, Scientific and Cultural

Organization, and was awarded a European Diploma of

Protected Areas (Category A) by the Council of Europe.

In 1994, a survey by the Greek Biotope/Wetland Centre

recorded 37 biotopes including 14 river estuaries, one

spring, one lake, six wetlands, nine rivers, three arti-

ficial lakes and three sealakes. Many sites in Crete

have been included in the Natura 2000 network and

many national and European projects have targeted the

protection, restoration and sustainable management of

these areas. A key issue of Cretan ecological protection

is the safeguarding of its water resources.

Water management in the past

In ancient times, water supply was covered by spring

and river water and shallow groundwater. Water storage

was achieved by a dense system of drainage networks

and cisterns. The complicated water supply and sewage

system of the Palace of Knossos was greatly admired

in prehistoric Crete, even though most of its features

were destroyed and little is known about its main opera-

tion. Some hypotheses assume that this system is the

complicated labyrinth mentioned in the Greek myths of

later periods. Aqueducts of gravity-flow and pressure-

piped systems were designed in the palace, revealing

a deep knowledge of water management techniques.

In the palace of Phaistos, terracotta pipes were in use,

comprising one of the earliest applications of hydro-

static law in communication vessels.

8

Today’s water resources balance

A mean annual precipitation of 934 mm corresponds to

a water volume of 7,700 hm

3

. Due to high temperatures

it is estimated that almost 72 per cent (5,544 hm

3

) of

the rainwater is subject to evapotranspiration, with only

12.5 per cent generating surface flow (962 hm

3

) and

15.5 per cent (1,194 hm

3

) filtering into the soil.

9

An

estimated 593 hm

3

of groundwater enters the surface

flow as spring water. The major springs are found in

the north-west part of Crete (maximum recorded flow

6,000 m

3

/hr) in contrast to the south-east part, where

springs flow at 15-70 m

3

/hr.

Annual freshwater needs in the Cretan region reach

515 hm

3

. Of this, human water supply demands around

Crete faces limited natural water supply and increased seasonal

demand, especially in the summer for agricultural and touristic

use. A key issue of concern is the allocation of water resources

to ensure sufficient water for all demands. During recent decades

several hydraulic projects such as reservoirs and water pipe systems

have been constructed to serve water needs, drastically altering the

natural regime of rivers and aquifers. There is a conflict between

users’ demand and the rational use and protection of the island’s

existing water resources.

The island of Crete

Greece covers an area of 130,000 km

2

in the Mediterranean region

in the south of Europe. The island of Crete occupies the southern

part of Greece with an area of 8,265 km

2

and is divided into four

prefectures: Lassithi (1,810 km

2

), Heraklion (2,626 km

2

), Rethymno

(1,487 km

2

) and Chania (2,342 km

2

). Agricultural areas cover 37.9

per cent of the island (3,134 km

2

). Permanent trees (mostly olive

and orange trees) occupy 1,901 km

2

, arable land 300 km

2

, vegeta-

bles and other horticultural crops 86 km

2

, grapes and raisins 255

km

2

, and 592 km

2

is fallow land. The permanent population of

the island is 601,131.

4

In 2006, the livestock population on the

island was counted as 2,000 heads of cattle, 65,000 pigs, around 1.3

million sheep, 635,000 goats, 6,000 horses, over 1 million heads of

poultry, 544,000 rabbits and 158,000 beehives.

Four mountain ranges run west to east: the White mountains in

the west (2453 m), Idis mountain (2,456 m) in the centre, Asterousia

(1,280 m) in south Irakleion and Dikti (2,148 m) in the east. The

geology of Crete is comprised of limestone, which allows water to

penetrate, creating major karstic formations.

5

Crete stands on the

verge of the tectonic trough of the Mediterranean and the Aegean

volcanic bow, giving the island high seismic activity.

Crete has a typical Mediterranean climate with cool winters and hot

summers. The mean annual temperature ranges from 18.5

o

C in the

Water storage in ancient Greece: an ancient courtyard with a

cistern in the foreground

Image: www.minoancrete.com/chamaizi.htm