Vízügyi Közlemények, 1988 (70. évfolyam)

2. füzet - Rövidebb tanulmányok, közlemények, beszámolók

A vízmércék magassági rendszerének kialakulása a Körösök völgyében 321 II. táblázat A 0 pontnál alacsonyabb vízállások A folyó neve Helység Legkisebb vízállás Év Fehér-Körös Honctő - 28 cm, 1987 Kőröskisjenő -200 cm, 1930 Gyula -210 cm, 1968 Fekete-Körös Nagyzerénd - 7 cm. 1968 Ant - 92 cm, 1986 Remete - 84 cm, 1968 Kettős-Körös Doboz - 26 cm, 1900 Békés -134 cm, 1946 Mezőberény -125 cm, 1975 Kőröstarcsa - 94 cm, 1935 Hármas-Körös Gyoma -116 cm, 1935 Árvízkapu -141 cm, 1984 Szarvas -148 cm, 1953 Békésszentandrás -200 cm, 1982 Kunszentmárton -240 cm. 1946 Bökény -285 cm, 1968 Sebes-Körös Csúcsa - 10 cm. 1986 Nagyvárad - 36 cm. 1987 Kőrösszakái -176 cm. 1983 Újiráz - 74 cm. 1983 Foki-híd - 70 cm. 1950 Kőrösladány - 68 cm, 1950 Berettyó Szilágynagyfalu - 40 cm. 1987 Pocsaj - 62 cm, 1972 Berettyóújfalu -166 cm, 1973 Darvas - 61 cm. 1962 Szeghalom - 59 cm. 1911 The history of the vertical arrangement of water stages in the Körös-Valley by 1. GÓG The geodetic levelling system needed for technical planning in the Tisza-Valley was set up by Mátyás Huszár before 1818. The base-point of the system was the lowest water level of the Tisza River at the city of Szeged ever experienced and labeled as 50 feet in altitude. The fixing of this level was realized at the water stage located beside the southern rondella of the castle of Szeged, just beside the water-bastion. Mr. Huszár took care also of the deployment of a series of fix points and had developed in this way the backbone of a levelling system. Flood levels were marked sometimes on the trunks of projecting trees (Fig. I). The oldest existing water stage (scaled according to feet and inches) has been found on the straight pillar of the 171 year-old bridge of the Elővíz-Canal (Fig. 2). In the years of 1842-43 a coordination of the levelling fix points was initiated and executed by Pál Vásárhelyi. The base-point was the average water level of the Adriatic Sea in the Gulf of Fiume. In this system, the „0" point of the water stage at Szeged received the value of 238'2"6"'.