List of geotopes in the district of Neuburg-Schrobenhausen
This list contains the geotopes of the Upper Bavarian district of Neuburg-Schrobenhausen in Bavaria . The list contains the official names and numbers of the Bavarian State Office for the Environment (LfU) as well as their geographical location. This list may not be complete. Around 3,400 geotopes (as of March 2020) are recorded in the Bavarian geotope register. The LfU does not consider some geotopes suitable for publication on the Internet. For example, some objects are not safely accessible or may only be entered to a limited extent for other reasons.
Surname | image | Geotope ID | Municipality / location | Geological unit of space | description | Area m² / extension m | geology | Digestion type | value | Protection status | comment |
---|---|---|---|---|---|---|---|---|---|---|---|
Former quarry N von Laisacker |
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185A001 |
Neuburg on the Danube position |
Southern Franconian Alb | The former quarry opens up a coral reef of the Malm Zeta 2–3 with transition to fossil-rich reef rubble banks. | 15000 150 × 100 |
Type: Sedimentary structures Type: Limestone |
Quarry | especially valuable | Natural monument, nature park | |
Finkenstein NW of the Bittenbrunn Danube barrier | 185A002 |
Neuburg on the Danube position |
Southern Franconian Alb | The rocky slope in the area of the Steppberg-Neuburger-Talenge, a breakthrough of the Danube through the Franconian Jura, uniquely opens up the most recent layers of the Malm in Bavaria: Zeta 5 (Rennertshofer layers), followed by the Neuburg bank limestone (Malm Zeta 6) . At the same time, the Neuburg Danube breakthrough is an important witness to the recent major river shifts in Bavaria. | 1000 50 × 20 |
Type: Layer sequence Type: Limestone |
Slope crack / rock wall | especially valuable | Nature reserve, landscape protection area, FFH area | ||
Former quarry at Unterhausen train station | 185A003 |
Oberhausen position |
Southern Franconian Alb | The profile shows the type locality of the Unterhausen and Oberhausen layers (Neuburg Bankkalke, Malm Zeta 6). These are the youngest preserved layers of the Malm in the Franconian Alb. The outcrop is rich in fossils, which already show an increasing influence of freshwater during sedimentation. | 12000 400 × 30 |
Type: Standard / Reference Profile, Animal Fossils, Layer Sequence Type: Limestone |
Quarry | especially valuable | Natural monument | ||
Rock slope in Bertoldsheim | 185A004 |
Rennertshofen position |
Donauried | The reef limestone of the upper Malm is well exposed above the local road. | 800 40 × 20 |
Type: Rock Type: Limestone |
Slope crack / rock wall | significant | Natural monument, nature park | ||
Outcrop N from Störzelmühle | 185A005 |
Rennertshofen position |
Riesalb | One of the few outcrops of the Malm Zeta 4. The Usseltalschists merge with the Rennertshofen strata upwards into the limestone. | 500 50 × 10 |
Type: Layer sequence Type: Limestone |
Quarry | especially valuable | Landscape protection area, nature park | ||
Former Sand pit SE von Rohrenfels | 185A006 |
Rohrenfels position |
Donaumoos | In the fine sands of the Upper Freshwater Molasse, thin sandstone banks with remains of flora and seeds as well as leaf prints have been preserved. There are only small residual outcrops. | 2500 50 × 50 |
Type: Vegetable Fossils Type: Sand, Sandstone |
Gravel pit / sand pit | significant | Natural monument | ||
Former Quarry NW of Bertoldsheim | 185A007 |
Rennertshofen position |
Riesalb | In the quarry, 12 m of the lower Rennertshofen layers are exposed. There is still a lime kiln in the former quarry. | 1000 50 × 20 |
Type: Standard / Reference Profile, Animal Fossils, Layer Sequence, Lime Kiln Type: Limestone |
Quarry | precious | Landscape protection area, nature park | ||
Ceiling ballast outcrop NE from Wengen | 185A008 |
Burgheim position |
Iller-Lech region | The profile shows a conglomerate of sandy gravel. This belongs to the terrace of the lower deck ballast in the Aindlinger terrace stairs. | 500 50 × 10 |
Type: Layer sequence, terrace Type: Conglomerate, gravel |
Quarry | precious | no protected area | ||
Former quarry W von Hütting | 185A009 |
Rennertshofen position |
Riesalb | Only the rear outcrop wall of the large dolomite quarry has been preserved. | 50000 250 × 200 |
Type: Rock Type: Dolomite Stone |
Quarry | significant | Landscape protection area, nature park, FFH area | ||
Former quarry N of walls | 185A010 |
Rennertshofen position |
Southern Franconian Alb | The former quarry opens up reef dolomite from the uppermost Malm (Malm Zeta 3–5). | 3000 100 × 30 |
Type: Rock Type: Dolomite Stone |
Quarry | inferior | Landscape protection area, nature park, FFH area | ||
Former chalk quarrying W von Neuburg | 185A011 |
Neuburg on the Danube position |
Southern Franconian Alb | Relatively large outcrops of pending Cretaceous sands on the edge of the former mining site. | 3000 150 × 20 |
Type: Rock Type: Sand |
Gravel pit / sand pit | significant | Landscape protection area, FFH area | ||
Former silica mining N of Riedensheim | 185A012 |
Neuburg on the Danube position |
Southern Franconian Alb | At the edge of the former silica mining, a small part of the mining wall was kept open. The bending of the limestone layers on the edge of the former deposit can be clearly seen. | 75 15 × 5 |
Type: Flexur Type: Limestone |
Quarry | precious | Landscape protection area, nature park | ||
Former Quarry W of Neuburg | 185A013 |
Oberhausen position |
Southern Franconian Alb | Slightly discordant marl-like limestone banks of the Malm Zeta 4 lie above the reef rubble limestone of the Malm Zeta 3. | 150 30 × 5 |
Type: Layer sequence, discordance Type: Limestone |
Quarry | precious | Landscape protection area, FFH area | ||
Former quarry N von Unterhausen | 185A014 |
Oberhausen position |
Southern Franconian Alb | The former quarry still has large residual outcrops in the Neuburg bank limestone. A sequence of slab of limestone is exposed, with individual marl layers and individual thick limestone banks in between. | 150 30 × 5 |
Type: Rock Type: Limestone |
Quarry | precious | Landscape protection area | ||
Strudel hole on Antonienberg S by Stepperg | 185H001 |
Rennertshofen position |
Southern Franconian Alb | The Strudelloch is a half-cave in the bulging slope of the Danube, which offers good access here. | 100 50 × 2 |
Type: karst halfway / natural bridge, impact slope, rock type: limestone |
cave | significant | Natural monument, landscape protection area, FFH area | ||
Grotto below the Arco-Schlößchen N von Neuburg |
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185H002 |
Neuburg on the Danube position |
Donaumoos | Partly dolomitized banked reef rubble limestone build the impact slope with the half cave on the Danube bank. | 200 10 × 20 |
Type: Shore / surf cave , impact slope, rock type: Limestone |
cave | significant | Natural monument, landscape protection area, bird sanctuary | |
Vineyard caves NW of walls |
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185H003 |
Rennertshofen position |
Southern Franconian Alb | The level cave system consists of 5 spacious individual caves that have repeatedly served people as living quarters. Many prehistoric and early historical bone finds as well as artifacts of the Neanderthals and finds from the Neolithic and the Bronze Hallstadt period attest to this. | 2420 121 × 20 |
Type: Karst horizontal cave Type: Dolomite stone |
cave | precious | Nature reserve, landscape protection area | |
Wellheimer dry valley (southern part) |
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185R001 |
Rennertshofen position |
Southern Franconian Alb | The Danube flowed through the Wellheim dry valley from the Pleistocene to the Rift Ice Age. The valley is famous for its dry heaths interspersed with dolomite rocks. | 5000000 5000 × 1000 |
Type: dry valley, breakthrough valley, impact slope Type: gravel, dolomite stone |
no information | especially valuable | Landscape protection area, nature park | |
Dunes NW of Gröbern | 185R002 |
Waidhofen position |
Danube-Isar hill country | Elongated, morphologically quite distinctive dunes. These are late to post-glacial drifting sand drifts that stand out from their surroundings as a steep chain of hills. | 120000 800 × 150 |
Type: Dune field Type: Sand |
no information | precious | no protected area | ||
Dune N of Waidhofen | 185R003 |
Waidhofen position |
Danube-Isar hill country | Relatively large drifting sand dune, which is partly overgrown with the typical local pine forest. | 15000 150 × 100 |
Type: Dune Type: Sand |
no information | significant | Natural monument | ||
Terrace E by Illdorf | 185R004 |
Burgheim position |
Iller-Lech region | The very eye-catching terrace east of Illdorf consists of lower gravel and is a step of the Aindlinger terrace staircase. | 25000 500 × 50 |
Type: Terrace Type: Gravel, Conglomerate |
no information | precious | Nature reserve | ||
Terrace near Eschling | 185R005 |
Burgheim position |
Iller-Lech region | The Eschlinger terrace consists of lower gravel and is a step of the Aindlinger terrace stairs. | 20000 500 × 40 |
Type: Terrace Type: amphibolite, conglomerate |
no information | precious | Nature reserve, FFH area | ||
Relic stones at St. Willibald's Chapel W von Attenfeld | 185R006 |
Bergheim position |
Southern Franconian Alb | The blocks are made of Cretaceous sandstone. According to legend, the water from the round holes in the blocks is said to heal eye diseases and never to dry out. | 6 3 × 2 |
Type: Relic Rock, Boulder Type: Sandstone |
block | significant | Natural monument, landscape protection area, nature park | ||
Limestone block near Karlshuld | 185R007 |
Karlshuld position |
Donaumoos | The round block of Malm mass limestone comes from the gravel pits in the Wurm Ice Age gravel near Nazibühl. The former natural monument is now in front of the Karlshuld Danube Museum. It is possibly a relic of the Tertiary ejection masses of the meteorite impact in the Ries that was exposed by erosion. | 1 1 × 1 |
Type: Boulder Type: Limestone |
block | significant | no protected area | ||
Quartzite blocks NW of walls | 185R008 |
Rennertshofen position |
Southern Franconian Alb | Several smaller blocks testify to the former distribution of Cretaceous sandstone. | 1 1 × 1 |
Type: Relic Rocks Type: Blocks |
block | significant | Landscape protection area, FFH area | ||
Rabenfels NE from Hütting | 185R009 |
Rennertshofen position |
Southern Franconian Alb | Striking rock formation in the younger reef dolomites of the Upper Malms on the slope of the Wellheim dry valley. | 800 80 × 10 |
Type: Rock Tower / Needle Type: Limestone |
Slope crack / rock wall | significant | FFH area, landscape protection area | ||
Castle rocks in Hütting |
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185R010 |
Rennertshofen position |
Riesalb | The relic of a castle wall is still preserved on the rock. | 2000 100 × 20 |
Type: rock castle, layer sequence type: dolomite stone |
Slope crack / rock wall | significant | FFH area, bird sanctuary, nature park | |
Dune near Sandhof | 185R011 |
Schrobenhausen position |
Danube-Isar hill country | Small, but relatively striking dune in the Paartal. Somewhat impaired at the edge by some smaller old mining sites. | 200 20 × 10 |
Type: Dune Type: Sand |
no information | significant | no protected area | ||
Dunes in the Hagenauer Forst SE by Sandizell | 185R012 |
Schrobenhausen position |
Danube-Isar hill country | Particularly long and particularly striking dunes. | 300000 3000 × 100 |
Type: Dune field Type: Sand |
no information | significant | no protected area |
See also
- List of nature reserves in the district of Neuburg-Schrobenhausen
- List of landscape protection areas in the district of Neuburg-Schrobenhausen
- List of FFH areas in the district of Neuburg-Schrobenhausen
Individual evidence
- ↑ Data source: Bavarian State Office for the Environment, www.lfu.bayern.de, Geotoprecherche (accessed on September 16, 2017)
Web links
Commons : Geotopes in the district of Neuburg-Schrobenhausen - collection of images, videos and audio files