GREEK TRANSBOUNDARY GROUND WATER BODIES WD EAST MACEDONIA (11)
In the Water District of East Macedonia (WD.11) determind fifteen (15) ground water bodys (GWB). They belong to the whole catchment of Strimonas river basin (GR.06). From the fifteen (15) GWB, four (4) charatcterized as transboundary ground water bodys (TGWB) and are the following (from west to east): Ano Poroia - Beles GWB - GR11FB080 Agistro GWB - GR110B020 Vrontous GWB - GR110B110 TRANSBOUNDARY GROUND WATER BODIES (GWB) Menikio - Falakro GWB - GR110B030
TRANSBOUNDARY GROUND WATER BODIES (GWB)
Ano Poroia - Beles GWB GR11FB080 Ano Poroia-Beles ground water body (GWB) is a fissure system. It belongs to Strymonas River Water Basin and its area is 287,22 km 2. In the GWB there is a number of contact fault springs. Springs water is used for drinking and irrigation. The fissure Ano Poroia Beles GWB GR11FB080 continues beyond the border of Greece to the Proterozoic Bulgarian GWB.
Ano Poroia - Beles GWB GR11FB080
Agistro GWB - GR110B020 Agistro ground water body (GWB) is a karstic system. It belongs to Strymonas River Water Basin and its area is 153,58 km 2. Precipitation is the main source of aquifer supply. In the GWB the discharge is carried out mainly from springs. Springs water is used for drinking and irrigation. The qualitative (chemical) and quantitative status is good. The karstic Agistro GWB - GR110B020 continues beyond the border of Greece to the karstic BG4G0000Pt1036 Bulgarian GWB.
Agistro GWB - GR110B020
Vrontous GWB GR110B110 Vrontous ground water body (GWB) is a fissure system. It belongs to Strymonas River Water Basin and its area is 436,72 km 2. Precipitation is the main source of aquifer supply. In the GWB there are a few springs. Springs water is used for drinking and irrigation. The qualitative (chemical) and quantitative status is good. The fissure Vrontous GWB- GR110B110 continues beyond the border of Greece to the Proterozoic BG4G0000C2020 Bulgarian GWB.
Vrontous GWB GR110B110
Menikiou - Falakrou GWB GR110B030 Menikio Falakro ground water body (GWB) is a karstic system. It belongs to Strymonas River Water Basin and its area is 1.007,61 km 2. Precipitation is the main source of aquifer supply. The qualitative (chemical) and quantitative status is good. The karstic Menikiou Falakrou GWB GR110B030 is not continue beyond the border of Greece
Menikiou - Falakrou GWB GR110B030
In the Water District THRACE (WD.12) determind eighteen (18) ground water bodys (GWB). From the eighteen (18) GWB, four (4) charatcterized as transboundary ground water bodys (TGWB) and are the following (from west to east): Orestiada GWB - GR12BT010 Potamoi - Stavroupoli GWB - GR120B090 Drosinio GWB - GR120B100 TRANSBOUNDARY GROUND WATER BODIES (GWB) Soufli - Didimoticho GWB - GR12BT150
Orestiadas GWB - GR12BT010 Orestiada ground water body (GWB) is an alluvial system. It belongs to Evros River Water Basin and its area is 835,16 km 2. Precipitation, Ardas and Evros rivers runoff are the main sources of aquifer supply.the annual renewable reserves are 60 x 10 6 m 3. In the GWB there is a big number of boreholes which are used for drinking and irrigation. The qualitative (chemical) and quantitative status is good. The alluvial Orestiada GWB GR12BT010 continues beyond the border of Greece to quaternary BG3G000000Q048 and to neogene BG3G000000N011 Bulgarian GWB.
Orestiada GWB - GR12BT010
Potamon Stavroupolis GWB GR120B090 Potamoi Stavroupoli ground water body (GWB) is a mixed (alluvial - karstic - fissure) system. It belongs to Nestos River Water Basin and its area is 2.416,34 km 2. Precipitation and Nestos river runoff are the main sources of aquifer supply. In the GWB system there are few boreholes and a number of contact fault springs which are used for drinking. The qualitative (chemical) and quantitative status is good. The mixed Potamon Stavroupolis GWB GR120B090 continues beyond the border of Greece to paleogene BG3G0000Pg3021 and proterozoic BG3G00000Pt039 Bulgarian GWB.
Potamoi Stavroupoli GWB GR120B090
Drosiniou GWB - GR120B100 Drosinio ground water body (GWB) is a fissure system. It belongs to Komotini-Loutro Evrou River Water Basin and its area is 976,53 km 2. Precipitation is the main source of aquifer supply. In the GWB there are number of springs which are used for drinking. The qualitative (chemical) and quantitative status is good. The fissure Drosinio GWB GR120B100 continues beyond the border of Greece to proterozoic BG3G00000Pt046 Bulgarian GWB.
Drosinio GWB - GR120B100
Soufliou - Didimotichou GWB GR12BT150 Souflio - Didimoticho ground water body (GWB) is a mixed (alluvial - fissure) system. It belongs to Evros River Water Basin and its area is 1.203,57 km 2. Precipitation, Erithropotamos and Evros river runoff are the main sources of aquifer supply. In the GWB there are boreholes which are used for drinking and irrigation. The fissure Souflio Didimoticho GWB GR12BT150 continues beyond the border of Greece to proterozoic BG3G00000Pt046 Bulgarian GWB.
Soufliou - Didimotichou GWB GR12BT150