Introduction

Physical and Socio-economic Description of Armenia

The Biological Diversity of Armenia

Endemic, relict, rare and threatened species in Armenia

Agrobiodiversity and Species of Economic Importance

Landscapes and Ecosystems of Armenia

Threats to, and Impacts on, Biodiversity in Armenia

Existing measures for biodiversity conservation

Existing capacity and programmes for conservation

Biodiversity Strategy for the Republic of Armenia

 

 
 
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Land surface
A wide range of soil types are found in Armenia (Map 5), including 14 main soils. However, the country is extremely poor in fertile lands suitable for agriculture. In the Ararat Valley clay or clay-sand soil predominates, and the land is generally wet and rocky. In contrast, mountain meadow soils have the highest humus content (up to 12%, average 9%), which compares favorably to humus content in other areas (4-9% in forests, and 2% in deserts).


Table 1.4 Physical and ecological changes in Lake Sevan caused by the decline in water levels

Indicators
Previous levels
Current levels
Decline in level (m)
0.0
19.2
Altitude (m)
1916.2
1897.0
Area of watershed (km 2)
3475
3647
Area of lake surface (km 2)
1416
1244
Maximal depth (m)
98.6
79.4
Average depth (m)
41.3
26.2
Volume of water (km 3)
58.4
33.5
Water exchage rate (yrs)
40.7
25.0
Water transparency (m)
14.3
4.5
PH
9.2
8.7
Total ions (g/m 3)
720
680
Dissolved oxygen (g/m 3)
6.0
2.0
Mineral nitrogen (g/m 3)
0.003
0.16
Total nitrogen (g/m 3)
0.07
0.64
Mineral phosphorus (g/m 3)
0.32
0.007
Total Phosphoros (g/m 3)
0.37
0.06
Bacteria (10 6 kl/ml)
0.4
1.0
Phytoplanton (g/m 3)
0.32
2.4
Biomas (gC/m 2/yr)
91.0
463.6
Primary production (Kkal/m 2/yr)
1000.0
5000.0
Microphytes (t 10 3/yr)
900.0
26.0
Zooplankton (g/m 3)
0.45
0.70
Zoobenthos (g/m 3)
3.38
11.0
Fish (t/yr)
1000.0
2400.0

Erosion has affected much of the soil in Armenia, generally as a result of human activities (including unsustainable use of croplands and overgrazing), and certain soil types (particularly those associated with meadows) have been strongly affected by human influence.

Main landscape zones

The mountainous nature of Armenia results in a series of highly diverse landscapes, with variations in geological substrate, terrain, climate, soils, and water resources. These landscapes support a great variety of habitats, which support distinctive flora and fauna, and different human use. Seven distinct landscape zones are described in Armenia: deserts, semi-deserts, dry steppes, steppes, woodlands, sub-alpine and alpine lands (Table 1.5; Map 6).

Table 1.5 Areas covered by different landscape zones
Landscape belts
Altiude range(m above sea level)
% of national territory
Deserts and semi-deserts
700-1300
10
Mountain steppes
1300
37
(wet grassland)
(375-700)
-
(dry gassland)
(1300-1600)
-
Forests,trees and scrubland
600-2500
20
Alpine and sub-alpine meadows
2100
28

· Deserts and Semi-deserts occur in the Ararat Valley and adjacent mountain slopes at altitudes of 1200-1300m, in the Vaik lowlands, and the Meghri gorge. Sand accumulations in the Arax area result in a desert landscape, which are also found in saline lowlands. In these landscapes climate is dry and continental, with hot summers and moderately cold winters. The soils are generally of the semi-desert grey type, and have been managed for cultivation over the last millennia. Cultivation has required intensive irrigation, and these areas now support fruit, vegetable, flower, and wine production, but have suffered major impacts from human activities.

· Dry mountainous steppes are found at higher altitudes than semi-deserts (above 1500m) in the Ararat Valley, and some other areas, but are also found at lower altitudes (above 800m) in the lowlands to the north-east of the country, which were originally forested. The climate in the dry steppes is characterized by warm, dry summers and mild winters. A range of soils are found, but in the Ararat Valley these lands are typically stony. Irrigation of dry steppes allows cultivation of crops, vegetables and fruit, and these landscapes have also suffered severe human impact.

· Mountain steppes are the dominant landscape for most of the country, particularly at altitudes above 1500m (and at altitudes up to 2000m in the north, 2400-2500m in the south). Meadow steppes occur in the highlands, while patches of forest also occur on ridge tops among steppes in the north-east and Sjunik regions. Climate is generally moderate, with warm, cool summers, and moderate or cold winters. Soils generally have a humus content of between 6-7%. Steppes are used for agriculture (including cultivation of crops, vegetables, frost-tolerant fruit trees (in lower altitudes) and fodder plants (in highland areas).

· Forests generally cover the mid-zone of mountains, occurring at altitudes between 500m and 2100m in the north (up to 2500m in the south). In central Armenia forests occur in small areas rather than as a continuous zone, and forests can be found on steep slopes, and other areas with limited human access. Soil types include red soil in the lowlands and forest gray soils in the highlands.

· Sub-alpine meadows occur at higher altitudes than steppes and forests, including highland mountain ranges. Climate is moderate with short, cool summers and long, cold winters. Much of the land here is meadow, with soils of high humus content.

· Alpine meadows occupy the highest altitudes above sub-alpine meadows (up to 3000m in the north, 3800m in the south). These meadows represent the principal pasturelands for the country, with meadow and alpine vegetation. Climatic conditions are severe, with long, cold winters, and annual temperatures average less than -40. Snow cover lasts up to 9 months, and permanent snows may occur in some areas.

· Azonal landscapes cover over 10% of the territory of the country, and occur independently of altitude (unlike the previously described landscapes). These include wetlands, as well as saline and alkaline lands, which cover about 25,000 ha, including areas in the Ararat Valley where the underground waters are close to the earth surface, resulting in water vaporization and salt precipitation. Upland wetlands are dominated by fresh (non-brackish) water, while lowland wetlands (particularly those around the River Arax) are usually drained in summer, resulting in high salinity.

 
 
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