마이텐베스‬에서 가장 멋진 ‪20‬개의 천연기념물

In the case of the Ebersberg well, the laboratory determined, according to archaeologist Bernhard Häck of the Bavarian State Office for Monument Preservation, that the well was constructed between 1441 and 1444 (or even slightly earlier) and used as a water source until it was covered over and forgotten in the 1950s/60s. "The well was therefore in use for over 600 years," Häck concluded.

New photos of the highlight

업데이트 04/2026: 샘물 주변 공간이 확장되었습니다. 나무 오두막에는 우물 통로의 조명을 켤 수 있는 스위치가 있습니다. 울타리에 문이 설치되어 자전거 도로에서 접근할 수 있습니다.

A new and interesting highlight is being created in the Ebersberg Forest

The roof of the medieval well is currently being rebuilt

A dead-ice basin is a dry, swampy, or water-filled depression formed by the melting of dead ice. Blocks of ice that break away from the glacier tongue during melting and remain there are called dead ice. Dead-ice basins in which a water-retaining layer has developed, or whose steep slopes sometimes extend below the groundwater level, are water-filled, swampy, or boggy. Their funnel shape allowed rain and meltwater to collect. These small bodies of water have experienced varying degrees of siltation and moor development, even within the same basin. The range of vegetation formations is very broad. It ranges from small reed beds to large sedge marshes, small sedge marshes, quaking grasslands, floating leaf and aquatic vegetation, transitional bogs, and even black alder swamps. Source: https://www.toteiskessel.de/uber-toteiskessel/was-ist-ein-toteiskessel/

이 우물은 최소 600년 되었습니다(C14 방법으로 측정됨). 누가 지었는지는 아직 불분명합니다. 에버스베르크 수도원, 공작 또는 "발트후페"라고 불리는 곳에 살았던 산림 감시원이 용의선상에 있습니다. 연구가 진행 중이며, 2024년에는 이 우물이 대중에게 공개될 예정이며 지하수 측정 지점으로 사용될 것이라고 합니다. 2026년 업데이트: 이제 우물에 접근할 수 있습니다. 조명이 우물 통로를 볼 수 있게 해줍니다.

Beautiful views on and around the Langweiher