List of natural monuments in the Hildburghausen district

In the list of natural monuments in the district of Hildburghausen , the natural monuments in the area of ​​the district of Hildburghausen in Thuringia are listed.

Natural monuments

No.	designation	Botanical name	location	District	Description / remarks	image
	Kirchberg		50 ° 26 '57.8 "  N , 10 ° 51' 34.6"  E	Brno / Thür.		Image wanted
	Trees along the road Eisfeld - Crock		50 ° 26 '13.2 "  N , 10 ° 53' 44.5"  E	Ice field		Image wanted
	Friedhofslinden Dingsleben		50 ° 26 '2.8 "  N , 10 ° 36" 0 "  E	Thing life		Image wanted
	Ottilien Chapel near Ehrenberg		50 ° 28 '42.6 "  N , 10 ° 39' 55.8"  E	Ehrenberg
	Einfürst (old mining, geological outcrop)		50 ° 21 '0 "  N , 10 ° 34' 54.1"  E	Eicha	A morphologically clearly visible basalt dike in the Keuper layers. It has a south-south-west - north-northeast facing strike. The Keuper deposits in the area can be assigned to the colored marls of the Middle Keuper.	Image wanted
	Tanzlinde		50 ° 22 '27.1 "  N , 10 ° 44' 16.4"  E	Ice houses		Image wanted
	Tanzlinde		50 ° 22 '38.6 "  N , 10 ° 43' 35.4"  E	Steinfeld		more pictures
	Source mountain hole		50 ° 22 '27.5 "  N , 10 ° 43' 24.6"  E	Steinfeld	The Bergloch is on the southern edge of the village of Steinfeld. It is a funnel-shaped water basin with an approximately circular shape. In the south-west corner of the Bergloch there is a relatively fresh break in from February 1999 at the bottom of the water basin. The karst spring pours constantly at an almost constant temperature of 14 ° C. The bottom of the spring funnel is covered with tufa.	Image wanted
	Fehrenbacher Switzerland		50 ° 30 '33.8 "  N , 10 ° 56' 59.6"  E	Fehrenbach	Fehrenbacher Schweiz is a section of the Biber valley on the road to Masserberg with striking rock formations. It consists of the conglomerate of Fehrenbach of the Goldlauter series of the Unterrotliegend. The conglomerate is composed almost entirely of slate mountain material, with quartzite phyllites from the core zone of the Schwarzburger saddle predominating.	Image wanted
	Upper Dambachtal - Hähnlesbrunnen		50 ° 27 '14 "  N , 10 ° 45' 58.3"  E	Gerhardtsgereuth		Image wanted
	Upper Dambachtal - Rüssenteich		50 ° 27 '42.5 "  N , 10 ° 44' 50.6"  E	Gerhardtsgereuth		Image wanted
	Triniusfelsen near Masserberg		50 ° 31 '53.4 "  N , 10 ° 56' 37.7"  E	Masserberg	It is a free-standing rock made of mica porphyrite that is partially overgrown. The mica porphyrite is brown-red to purple or gray in color. In a finely crystalline to dense matrix there are light - fresh as well as partially decomposed - feldspars and biotite. The Trinius rock is the result of erosion. Sometimes the rock is more fractured.	Image wanted
	Mulberry tree		50 ° 22 '22.8 "  N , 10 ° 36' 13.3"  E	Gleichamberg		Image wanted
	Old oak on Dingslebener Strasse		50 ° 24 '53.3 "  N , 10 ° 34' 10.2"  E	Haina		Image wanted
	Three old linden trees on the boiler lawn		50 ° 25 '4.1 "  N , 10 ° 31' 56.6"  E	Haina		Image wanted
	Gun oak	Quercus robur	50 ° 16 '58.8 "  N , 10 ° 43' 39.4"  E	Heldburg
	Devil's Oak near Hellingen		50 ° 16 '4.1 "  N , 10 ° 41' 2.8"  E	Hellingen		Image wanted
	Burkhardt's source		50 ° 30 '53.6 "  N , 10 ° 34' 55.6"  E	Henfstädt	The source emerges in the immediate vicinity (2 m) of the Werra at the foot of a shell limestone rock face. The source outlet is framed with processed limestone.	Image wanted
	Stone church		50 ° 30 '52.2 "  N , 10 ° 35' 52.4"  E	Henfstädt		Image wanted
	Finch grove		50 ° 24 ′ 56.5 "  N , 10 ° 45 ′ 23"  E	Birch field		Image wanted
	Cemetery trees in Heubach		50 ° 30 '17.6 "  N , 10 ° 55' 35"  E	Heubach		Image wanted
	Copper beech at Bertholdstor		50 ° 25 '37.2 "  N , 10 ° 43' 57"  E	Hildburghausen
	Oak at middle school		50 ° 25 '40.4 "  N , 10 ° 43' 37.2"  E	Hildburghausen		Image wanted
	Two oaks in the Peace Park		50 ° 25 '26.8 "  N , 10 ° 43' 36.8"  E	Hildburghausen
	Chirotherium plates		50 ° 25 '34 "  N , 10 ° 43' 47.3"  E	Hildburghausen	In the Hildburghausen area, the chirotheria sandstone is a light, less clayey, even and fine-grain sandstone. It is almost always spotted brown or yellow (tiger sandstone) and occurs in strong banks. Numerous net strips (filled, former dry cracks) as well as wave furrows (ripples) occur in the chirotheria sandstone. A large plate with undulating ripples represents today's surface natural monument.
	High moor		50 ° 27 ′ 15.5 "  N , 10 ° 42 ′ 56.2"  E	Hildburghausen	The originally protected area is no longer detectable in the terrain (dried out), three small-area parts, mostly as source points in TCs, only shown over a large area in the KOMPASS hiking map (online).	Image wanted
	Cat sticks		50 ° 26 '34.1 "  N , 10 ° 41' 37.3"  E	Häselrieth	Einbach and Kohlbach flow into the Werra near the Katzenhölzchen . The Katzenhölzchen is - like the Lohmüllersteich and the Römersbachanlage (since 1957) - a protected natural monument. The stone cross there, the Katzenstein, is worth seeing .	Image wanted
	Römersbachanlage		50 ° 26 '15.4 "  N , 10 ° 43' 34.1"  E	Hildburghausen		Image wanted
	Lohmüllersteich		50 ° 26  '21.8 " N , 10 ° 43' 36.8"  E	Hildburghausen	Along the Römersbach, the path leads north past the Lohmüllersteich . Turn left at the wayside cross (Lohmüller's grove). After a few steps, the forest at the Charlottenbrunn opens up and opens up a view of the nearby Waldstadt ... residential area. The pond is located in a wooded area, it is only shown in full on the KOMPASS hiking map (online).	Image wanted
	Sheep oak		50 ° 26 '17.5 "  N , 10 ° 44' 45.6"  E	Hildburghausen		Image wanted
	Linden group Rondell		50 ° 24 '48.2 "  N , 10 ° 41' 27.6"  E	Leimrieth		Image wanted
	Field stone		50 ° 31 '39.7 "  N , 10 ° 38' 4.2"  E	Lengfeld		Image wanted
	Linden tree near linden trees		50 ° 20 '25.8 "  N , 10 ° 36' 18.4"  E	Linden trees		Image wanted
	Linden group on the street Linden - Gleicherwiesen		50 ° 20 '57.8 "  N , 10 ° 36" 43.9 "  E	Linden trees		Image wanted
	Weidenallee in Friedrichshall		50 ° 14 '58.9 "  N , 10 ° 45' 49"  E	Friedrichshall		Image wanted
	Oak in monk wood		50 ° 23 '53.5 "  N , 10 ° 29" 19.7 "  E	Mendhausen		Image wanted
	Linden tree in the Mönchshof		50 ° 23 '28.3 "  N , 10 ° 28' 49.8"  E	Mendhausen		Image wanted
	Oak		50 ° 22 '46.9 "  N , 10 ° 32' 15.4"  E	spleen		Image wanted
	Gallows ponds of the Wiedersbach near Poppenwind / Wiedersbach		50 ° 28 '0.8 "  N , 10 ° 49' 27.1"  E	Poppenwind		Image wanted
	Wellspring		50 ° 27 '19.4 "  N , 10 ° 38' 40.9"  E	Reurieth	The karst spring emerges on the western edge of the Werra valley in the area of ​​a north-north-west - south-south-east trending fault. The catchment area of ​​the karst spring comprises the shell limestone area west and south of Reurieth. The spring discharge is on average 200 l / s.	Image wanted
	Friedenslinde		50 ° 27 '10.1 "  N , 10 ° 39' 10.8"  E	Reurieth		Image wanted
	Friedhofslinden		50 ° 27 '11.2 "  N , 10 ° 39' 19.4"  E	Reurieth		Image wanted
	Old oak "on the pan"		50 ° 23 ′ 49.2 "  N , 10 ° 34 ′ 21"  E	Römhild		Image wanted
	Trees in the castle courtyard		50 ° 23 '52.1 "  N , 10 ° 32' 28.3"  E	Römhild		Image wanted
	Trees at the cemetery		50 ° 23 ′ 51 ″  N , 10 ° 32 ′ 15 ″  E	Römhild		Image wanted
	Chestnuts at the Hartenburg		50 ° 24 '9.7 "  N , 10 ° 33' 52.2"  E	Römhild		Image wanted
	Lindenallee on Friedrich – Höfling – Straße		50 ° 23 '44.5 "  N , 10 ° 32' 24"  E	Römhild		Image wanted
	Two linden trees on the Römhild - Irmelshausen footpath		50 ° 23 '17.5 "  N , 10 ° 30' 42.1"  E	Römhild		Image wanted
	Climbing leather oak		50 ° 23 '7.8 "  N , 10 ° 33" 33.8 "  E	Römhild		Image wanted
	Eibenhorst		50 ° 27 '15.1 "  N , 10 ° 57' 27.4"  E	Sachsenbrunn	One of the last large-scale yew occurrences in Thuringia is located north of the Schwarzenbrunn district.	Image wanted
	Meat tree		50 ° 26 '14.6 "  N , 10 ° 57' 27.4"  E	Sachsenbrunn		Image wanted
	Tanzlinde	Tilia platyphyllos	50 ° 26 '38.4 "  N , 10 ° 56' 40.5"  E	Sachsenbrunn
	Stalactite cave		50 ° 27 '14.8 "  N , 10 ° 58' 1.6"  E	Sachsenbrunn		Image wanted
	Sterzing beech		50 ° 31 '16.7 "  N , 10 ° 52' 18.1"  E	Schönbrunn (sluice ground)		Image wanted
	Mühlberg (and) Köpfle		50 ° 31 '37.9 "  N , 10 ° 53' 11"  E	Sachsenbrunn	The Mühlberg is located in the border area between the Thuringian Forest and the Thuringian Slate Mountains. Phyllitic slate is exposed on the head. This shows intense wrinkling.	Image wanted
	Pine near St. Bernhard		50 ° 27 '22.3 "  N , 10 ° 35' 57.1"  E	St. Bernhard		Image wanted
	Source		50 ° 26 ′ 47 "  N , 10 ° 59 ′ 30.1"  E	Stilts
	Heaven		50 ° 24 '23 "  N , 10 ° 43' 16.3"  E	Stressenhausen		Image wanted
	Kapellenberg		50 ° 23 '5.6 "  N , 10 ° 41' 0.6"  E	Stressenhausen	At the Kapellenberg there are layers of the Lower Gipskeuper series of the Middle Keuper. They are colorful marls with stone marl layers, dolomites, sandstones and quartz breccias. The Keuper deposits are broken through by a basaltic corridor (Limburgite) on the Kapellenberg. The corridor is no longer open, but there are reading stones.	Image wanted
	Linden tree at the entrance to Sülzdorf		50 ° 24 '40.3 "  N , 10 ° 29' 32.3"  E	Sülzdorf		Image wanted
	Occurrence of the Märzenbeche on the Red Wood		50 ° 24 '56.9 "  N , 10 ° 32' 37.3"  E	Sülzdorf		Image wanted
	Fall wall of the collapsed mountain		50 ° 29 '25.1 "  N , 10 ° 37' 16.7"  E	Themar	The landslide on the fallen mountain (80 m high, 500 m long) occurred on April 3, 1595. Here the Lower Muschelkalk, with its fissured limestones, is deposited on the claystones of the Upper Buntsandstein (Röt) are dammed up, the clay and marl stones of the Röt are soaked, which cause the hanging layers of the lower shell limestone to slide.	Image wanted
	Rappsgrabenschlucht		50 ° 14 '30.1 "  N , 10 ° 48' 46.4"  E	Ummerstadt	In the Rapsgraben Gorge, sandstones, claystones and limestones are cut, which can be assigned to the colorful Keuperletten with white sandstone banks (Middle Keuper 6) and the Dolomitic arcs (Middle Keuper 7). It is a gorge-like gorge.	Image wanted
	Trees at the old cemetery		50 ° 24 ′ 21.2 "  N , 10 ° 48 ′ 41"  E	Veilsdorf		Image wanted
	Eibenhorst		50 ° 24 '41.8 "  N , 10 ° 50' 10.7"  E	Schackendorf	A unique population of yew trees can be found in the “Schakendorfer Leite” nature reserve. The northern slope offers very good growth conditions for the more than a thousand yew trees on an area of ​​around 15 hectares.	Image wanted
	jaw		50 ° 25 '16.3 "  N , 10 ° 49' 33.2"  E	Schackendorf		Image wanted
	Linden tree		50 ° 24 '58 "  N , 10 ° 49' 17.8"  E	Schackendorf		Image wanted
	Linden tree at the church		50 ° 24 '29.2 "  N , 10 ° 48' 43.6"  E	Veilsdorf		Image wanted
	Grove of trees in the Börnersgrund near Waldau		50 ° 30 '19.1 "  N , 10 ° 49' 6.6"  E	Waldau		Image wanted
	Yew tree at the Westenfeld school		50 ° 25 '53.4 "  N , 10 ° 29' 46.7"  E	Westenfeld		Image wanted
	Linden tree on Sülzdorfer Strasse		50 ° 25 '41.9 "  N , 10 ° 29' 46.7"  E	Westenfeld		Image wanted
	Wild - women - holes		50 ° 26 '49.2 "  N , 10 ° 29' 9.6"  E	Westenfeld	It is a notch valley with the former cave entrance on the slope. The entrance to the cave is filled with rock. The karst hollow was created by carbonate dissolution and leaching. The tectonic stress caused by the bulging of the Bibra saddle contributed to the formation of the cave. There are two abandoned quarries in the Lower Muschelkalk on the eastern slope of the valley.	Image wanted
	Oak in the master peg		50 ° 18 ′ 31.3 "  N , 10 ° 40 ′ 43.3"  E	Westenfeld		Image wanted
	Crypt oak near Haubinda		50 ° 20 '23.3 "  N , 10 ° 38' 8.5"  E	Haubinda		Image wanted
	Niederungsmoor of the Wiedersbach		50 ° 28 '23.9 "  N , 10 ° 49' 3.4"  E	Wiedersbach		Image wanted
	Oak		50 ° 24 '46.4 "  N , 10 ° 37' 25.3"  E	Zeilfeld		Image wanted
	1 red beech and 2 hornbeams			Eichenberg		Image wanted
	Spring spring area		50 ° 25 '37.9 "  N , 10 ° 32' 37.3"  E	Haina	The source emerges at the border between Lower and Middle Muschelkalk. The karst spring is built over with a spring house and has a free overflow.	Image wanted
	Linden and oak trees in the old quarry		50 ° 22 '27.8 "  N , 10 ° 33' 44.6"  E	Hindfeld		Image wanted
	The big stone north of Gießübel		50 ° 34 '20 "  N , 10 ° 55' 23.4"  E	Pouring evil	The Große Stein is located on the northern outskirts of Oberneubrunn on the steeply rising south and south-west slope of the summer mountain. On the summit of the Großer Stein, a boulder with heavily folded rock protrudes. It is an intensely folded slate and quartzite with a strong phyllitic sheen. In the phyllites, layers or crooks of fatty quartz, graphitic slate, amphibolite and porphyroid (slated porphyry) can generally be embedded.
	Village linden		50 ° 23 '15.7 "  N , 10 ° 39' 20.2"  E	Bedheim
	Oak		50 ° 26 '38.4 "  N , 10 ° 40' 44.4"  E	Ebenhards		Image wanted
	Oak near Ehrenberg		50 ° 29 '8.5 "  N , 10 ° 40' 3.4"  E	Ehrenberg		Image wanted
	buckeye		50 ° 25 '3.4 "  N , 10 ° 53" 52.1 "  E	Ice field		Image wanted
	Seven oaks		50 ° 16 ′ 57.7 "  N , 10 ° 41 ′ 45.2"  E	Gellershausen		Image wanted
	Juniper trees		50 ° 17 '32.6 "  N , 10 ° 41' 40.9"  E	Gellershausen		Image wanted
	Linden tree on the monument square		50 ° 22 '27.8 "  N , 10 ° 35' 49.6"  E	Gleichamberg		Image wanted
	Linden tree at the Israeli cemetery		50 ° 21 '25.9 "  N , 10 ° 38' 20"  E	Equally proven		Image wanted

See also

• List of nature reserves in the Hildburghausen district
• List of cultural monuments in the district of Hildburghausen

Web links

Commons : Natural monuments in the district of Hildburghausen  - Collection of images, videos and audio files

• Thuringian environmental portal map service

supporting documents

1. ↑ Natural monuments (ND) and area natural monuments (FND) - § 16 ThürNatG. www.landkreis-hildburghausen.de, accessed on May 16, 2016 .  
2. ↑ ^{a b c d e f g h i j k l m n} N.N .: Maps. Thuringian Ministry for the Environment, Energy and Nature Conservation, accessed on January 7, 2019 .  

 Map with all coordinates: OSM | WikiMap