List of geotopes in the Aichach-Friedberg district
This list contains the geotopes of the Swabian district of Aichach-Friedberg 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 Gravel pit N by Gumpenberg | 771A001 |
Pöttme's position |
Iller-Lech region | The Gumpenberg gravel pit closes the oldest Pleistocene gravel of the Aindlinger terrace stairs. It is largely fused. | 5000 100 × 50 |
Type: Rock Type: Gravel |
Gravel pit / sand pit | precious | no protected area | ||
Former Clay pit NE by Froschham | 771A010 |
Aichach position |
Danube-Isar hill country | The clay pit was operated by the Renz brickworks in Aichach until 2002. At that time, clays, silts and fine sands of up to 25 m in thickness from the older series were open. The fine sediments were divided by paleo soils. Most of the groundwater has flooded the pit, only in the north a 3 m high outcrop remained. | 105000 300 × 350 |
Type: Rock, Fossil Soil Type: Clay, Sand |
Clay pit / clay pit / marl pit | significant | no protected area | ||
Paleo soil in Altgraben S von Dasing | 771A011 |
Friedberg position |
Danube-Isar hill country | Humus paleo-soil, which is covered by silty-sandy floodplain deposits. It is about 1.8 m below ground level on the Altgraben south of Dasing, which has been artificially straightened and cut up to 2 m into the valley floor. Using ceramic shards from the Latène and Roman times, the former valley floor can be dated to the first millennium BC. | 800 400 × 2 |
Type: Fossil Soil, Trench, Canal Type: Clay |
Slope crack / rock wall | significant | FFH area | ||
Immendorf sand pit N | 771A012 |
Pöttme's position |
Donaumoos | In the Immendorf sand pit , diagonally layered fine sands of the Upper Freshwater Molasse are exposed . In the sand reprocessing documents and Tongerölle are seen in nest sand martins . A 3 to 4 m thick silt layer with limestone concretions lies above the fine sand . | 3500 70 × 50 |
Type: Rock Type: Sand |
Gravel pit / sand pit | significant | no protected area | ||
Mine field Grubet NE from Oberschneitbach | 771G001 |
Aichach position |
Danube-Isar hill country | Large excavation pit from the early to high Middle Ages with approx. 3500 pings . Iron ore concretions were exploited in the Upper Freshwater Molasse. | 200000 1000 × 200 |
Type: Pinge field Type: Iron / manganese ore, gravel, sand |
Ping | precious | Ground monument | ||
Source outlet Silberbrünnle S from Notzenfeld | 771Q001 |
Aichach position |
Danube-Isar hill country | The name of the stream goes back to light mica in the stream sediment (sands of the upper freshwater molasses). There are heavy mineral soaps (mainly garnet ) in the stream bed . The springs rise above tertiary clay, above which water-bearing sands of the older series stand. | 280000 700 × 400 |
Type: Layer spring, hillside spring moor Type: Sand, peat |
no information | significant | Landscape protection area | ||
High terrace NE of Unterbergen | 771R001 |
Schmiechen position |
Paar-Isar region | Elevated terrace from the Riss glaciation , which ends to the north. | 65000 2600 × 25 |
Type: Terrace Type: Gravel |
no information | significant | no protected area | ||
Paartal SW of Ottmaring | 771R002 |
Friedberg position |
Danube-Isar hill country | The Paartal was created by the backward erosion of the Lower Couple, which in the early Holocene merged with the Upper Couple, which flows on the east side of the Lech Valley , to form today's course. | 150,000 600 × 250 |
Type: Sohlental Type: gravel, sand |
no information | precious | Natural monument, landscape protection area, FFH area | ||
Upper Schindbachtal W from Griesbeckerzell | 771R003 |
Aichach position |
Danube-Isar hill country | The valley of the Schindbach changes downstream from a Muldental to a sole valley . Spring niches and spring horizons on the slopes lead to swamping. | 100000 500 × 200 |
Type: Asymmetrical Valley, Mulde Valley, Layer Source Type: Sand |
no information | significant | Landscape component | ||
Impact slopes on the pair S of Dasing | 771R004 |
Friedberg position |
Danube-Isar hill country | Impact slopes formed by the meandering couple south of Dasing in fine tertiary sands of the Middle Series. | 100000 500 × 200 |
Type: Prallhang, Meander Type: Sand |
Impact slope / river bed / stream profile | significant | FFH area | ||
Malmkalkblock in Oberbaar | 772R003 |
Baar position |
Iller-Lech region | Large chunk of mass limestone found in the gravel pit northeast of Thierhaupten . It is the largest known block of gravel slabs. It is either a Reuter's block (by Ries event transported) or a drift block in the course of the Danube during the Early Pleistocene . | 2 2 × 1 |
Type: Ejecta Material (Impact), Rock Type , Boulder Type: Limestone |
block | significant | no protected area |
See also
- List of nature reserves in the Aichach-Friedberg district
- List of landscape protection areas in the Aichach-Friedberg district
- List of FFH areas in the Aichach-Friedberg district
Individual evidence
- ↑ Data source: Bavarian State Office for the Environment, www.lfu.bayern.de, Geotoprecherche (accessed on September 16, 2017)