History
In the picturesque valley, which is bordered on the north by the Krupina Highlands, on the south by the Börzsöny Mountains, on both sides of the river Ipeľ lies the town. At this point, the valley is the narrowest: the distance between the two mountains is less than 3 kilometers. In the middle of this valley flows Ipeľ. The rich growth growing on the banks and the proximity of forests provided ideal conditions for the settlement of prehistoric man. Archaeological excavations testify that even in the Late Stone Age (Early Palaeotic) man lived here / 1 /, from the Krupinica stream to Parasso - today's customs area of the Slovak-Hungarian border.
The climate here is dry and warm, characterized by relatively short winters and long, above-average warm summers. The number of summer days (tmax at 25´C) is over 70, the average annual temperature is 9.5´C. The average precipitation for the growing season shows a deficit, which means that the evaporation is greater than the total precipitation. Fluctuations in precipitation are caused by the fluctuations of the Ipľa flow water. In the summer months, when moisture is most needed, it reaches barely 20m3 / sec, while in March it reaches up to 58m3 / sec.
Geologically, the river valley originated in the Neogene, when the still continuous Börzsöny and Krupinská mountains parted as a result of strong rock movement, and the sea penetrated here as the valley fell. Later, with the decline of the sea, the entire Danubian lowland also decreased, which had an impact on the occurrence of large erosion in the Poiplí, which created river terraces. These are well visible on the Calvary Hill and on the conglomerate terraces behind the cemetery. In the Miocene, volcanic activity took place in our area, the epicenter of which was probably in the Krupina Highlands. Our vineyards "Nagyszőlők" are also of volcanic origin, where quality wine is born. Near the town, the flow of the river slows down considerably and, due to the shallowness of the banks, it exits the riverbed several times a year. Here, solid parts of the earth's crust, washed away by erosive activity from the upper reaches, settle. The thickness of the sediment thus formed also reaches 4-7 m. Different types of sedimentary soils were formed on them.
The first written mention of the existence of the Saag settlement is from 1237 in the document of Bela IV., Written in Zvolen. In it, the Esztergom church, owned by two and a half plowed lands and one mill in the Saag district, belonging to the Hont castle, confirms. The second document from 1256 describes the settlements adjacent to the Shahs: the village of Olvár, the village of Tešmak, the village of Proma and Sági-sidó (on the site of today's Kómájszőlő). At that time, according to the mentioned document, Peter Viski, Rugas' son Egyed, as well as castle subjects and royal servants, royal courtmen, the Esztergom chapter and the Shah's post office were also the owners of land in the Shah.