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Saalehöhle

A 35 m long collapse doline cave in heavily jointed calcareous marls and marly limestones; the fenced entrance leads into a stepped chamber whose shaft floor was once covered by a large rubbish heap.

Lichtenau

A 35 m long collapse doline cave in heavily jointed calcareous marls and marly limestones; the fenced entrance leads into a stepped chamber whose shaft floor was once covered by a large rubbish heap.

特征

洞穴是受保护的生境(§30 BNatSchG)。蝙蝠用作越冬场所的洞穴,每年10月1日至3月31日禁止进入(§39(6) BNatSchG),但观光洞穴及其已开发部分除外。

位置

The cave lies within the wooded right valley slope of the Sauer about 200 m above the dam of the retention basin, about 20 m west-northwest of the path and about 70 m south-southeast of the junction.

地图

大致位置

洞口

出发前请务必核对坐标和通行条件。

  1. Saalehöhle

    51.609293, 8.815991
下载所有洞口的 GPX

描述

形态

It is a 35 m long collapse doline cave within the heavily jointed calcareous marls and marly limestones of the Oerlinghausen Formation (Middle Turonian, formerly "lamarcki beds"). The right chamber is stepped. The rock cavity on the right appears to have been formed by corrosion.

水文

When the Sauer level still lay several metres higher, the Sauer from Atteln made a bend to the north. Possibly there is an old sinkhole near the cave.

行进路线

The shaft floor consisted of a large rubbish heap that allows narrow squeeze-through passages between rubbish and rock in two directions. The rubbish has since been removed. The cave entrance is fenced.

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来源:Geotopkataster Nordrhein-Westfalen (Geologischer Dienst NRW)(ogc-api.nrw.de),已修改。 Data licence Germany – attribution – version 2.0 (dl-de/by-2-0), https://www.govdata.de/dl-de/by-2-0 Geowissenschaftliche Daten: INSP-GeotopeinNRW @ Geologischer Dienst NRW · 2026年数据