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56-738: In addition, Rügener Kreide is the trade name for the white pigment that is extracted from these limestones. Lithostratigraphically , the Rügen chalk belongs to the Hemmoor Formation of the Chalk Group and is formally defined as the Rügen Member within this formation. Chronostratigraphically , the Rügen Member falls into the late lower to late upper Lower Maastrichtian (approx. 70 million years ago). Chalk widely occurs in

112-507: A GDR standard excavator of the 1960s and 1970s. Both the raw chalk and the debris were transported by railways. With the completion of this plant in 1962 (initially trial operation, from 1963 regular production) the production time from excavation to shipping was reduced to only 80 minutes. Until then, it was up to 80 days. The chalk lorries and the excavators later became larger (UB 162-1), and on an experimental basis, 20-m lorries designed for lignite open pit mining were also used in

168-423: A barrier. The results are presented as a correlation scheme (A). Practical correlation has a lot of difficulties: fuzzy borders of the layers, variations in composition and structure of the rocks in the layer, unconformities in the sequence of layers, etc. This is why errors in correlation schemes are not seldom. When the distances between available cross-sections are decreasing (for example, by drilling new wells)

224-627: A dozen excavators were in operation during chalk mining. From the Jasmund quarries, the rough chalk came either via a railway line, the Kreidebahn , to Martinshafen near Sagard (there are also old quarries) or with a cable car to the Port of Sassnitz. The chalk railway forked towards the mining area into a northern and a southern section of the line. The southern line ran from Wittenfelde via Klementelvitz and Quatzendorf to Marlow, where it merged with

280-479: A lithostratigraphic unit includes a stratotype which is usually a type section . A type section is ideally a good exposure of the unit that shows its entire thickness. If the unit is nowhere entirely exposed, or if it shows considerably lateral variation, additional reference sections may be defined. Long-established lithostratigraphic units dating to before the modern codification of stratigraphy, or which lack tabular form (such as volcanic domes), may substitute

336-677: A mountain landscape. To the north and east the Granitz is bounded by a cliffed coast on the Baltic Sea. In the south it adjoins the Mönchgut region and in the north, the narrow bar of the Schmale Heide . The 23-acre (9.3 ha) Black Lake ( Schwarzer See ) lies in the Granitz as do several kettle bogs . A number of non-native stands of conifers are being turned into a near-natural forest. No roads of any description run through

392-450: A type locality for a type section as their stratotype. The geologist defining the unit is expected to describe the stratotype in sufficient detail that other geologists can unequivocally recognize the unit. Lithosome : Masses of rock of essentially uniform character and having interchanging relationships with adjacent masses of different lithology . e.g.: shale lithosome, limestone lithosome. The fundamental Lithostratigraphic unit

448-470: A water content of 30 to 35%. This heavy, mass was then knocked out , that is, it was shoveled out of the settling basins into carts. The workers who carried out the work steps from dismantling to knocking out were called sludgers . Other workers, the so-called formers , transported the wet chalk with the carts to the dry sheds , and formed the chalk into shovel-sized masses and laid them out there for drying. The chalk had to be relayered several times during

504-596: Is a wooded ridge in the southeast of Germany's largest island, Rügen , between the Baltic Sea resorts of Binz and Sellin . The woods cover an area of 982 hectares and are designated as a nature reserve . Since 1991 they have been part of the Southeast Rügen Biosphere Reserve . Characteristic of the Granitz are its rich stands of beech and sessile oak and its rolling landscape of push end moraines , which in some ways resemble

560-449: Is called an unconformity . Four types of unconformity: To correlate lithostratigraphic units, geologists define facies, and look for key beds or key sequences that can be used as a datum. Geological correlation is the main tool for reconstructing the geometry of layering in sedimentary basins . The lithological correlation is a procedure, decisive what layers (strata) in geological cross-sections located in different places belong to

616-626: Is given a geographical name combined with either a rock name or some term describing its form. The term suite is deprecated. Also formalized is the term complex , which applies to a body of rock of two or more genetic classes (sedimentary, metamorphic, or igneous). This establishes two hierarchies of lithodemic units: Similar rules have been adopted in Sweden. However, the 1994 International Stratigraphic Guide regards plutons and non-layered metamorphic rocks of undetermined origin as special cases within lithostratigraphy. Granitz The Granitz

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672-469: Is in the form of micrometer-sized low-Mg calcite platelets, so-called coccoliths , which are remnants of unicellular , planktonic calcareous algae, so-called coccolithophores . The calcareous algae lived around 70 million years ago in the light-flooded surface water of a sea that covered northern Germany. After their death, they sank to the bottom of the sea and, over time, formed huge deposits of limestone mud. This lime sludge has come down to us today in

728-423: Is increasingly being offered as a so-called healing chalk for mud packs and other applications. Lithostratigraphy Lithostratigraphy is a sub-discipline of stratigraphy , the geological science associated with the study of strata or rock layers. Major focuses include geochronology , comparative geology, and petrology . In general, strata are primarily igneous or sedimentary relating to how

784-467: Is relatively crumbly but still brittle , water-saturated Rügen chalk is more plastic , almost like moist clay , and can be cut with a knife. Like many other limestones of the Upper Cretaceous, the Rügen chalk has a very high content of calcium carbonate (CaCO 3 , "carbonate of lime"). With the Rügen chalk the calcium carbonate content is at least 97%. The vast majority of calcium carbonate

840-413: Is the formation . A formation is a lithologically distinctive stratigraphic unit that is large enough to be mappable and traceable. Formations may be subdivided into members and beds and aggregated with other formations into groups and supergroups. Two types of contact: conformable and unconformable . Conformable : unbroken deposition, no break or hiatus (break or interruption in the continuity of

896-563: The VEB Vereinigte Kreidewerke Rügen after 1957. By 1945, the dismantling has been stopped in the oldest quarries on the eastern edge of the Jasmund and at Lohme , as well as in the quarries from Dumsevitz , Rosengarten and Altkamp Südrügen. With the completion of a large and modern chalk works in Klementelvitz between Sassnitz and Sagard , many other smaller chalk quarries were closed after 1962 and

952-535: The Soviet occupation zone and later to the GDR meant the elimination of private economic structures in the Rügen chalk industry for the next 45 years. It was only in this period that modern technology completely replaced strenuous physical work in many areas. Since chalk was soon in demand again as a raw material with the reconstruction, a total of 19 chalk quarries started operations on Rügen after 1945, which were combined in

1008-419: The subsurface of Northern Germany, but is largely overlain by several hundred metre thick Cenozoic deposits. Chalk limestones are often layered. The Rügen chalk, however, is unlayered and massive. The rock is extremely fine grained and very low cementation , which is associated with a high porosity . The low cementation and high porosity mean that the rock can soak up a lot of water. While dry Rügen chalk

1064-523: The Danish naturalist, Nicolas Steno , in his 1669 Dissertationis prodromus . A lithostratigraphic unit conforms to the law of superposition , which in its modern form states that in any succession of strata , not disturbed or overturned since deposition , younger rocks lies above older rocks. The principle of lateral continuity states that a set of bed extends and can be traceable over a large area. Lithostratigraphic units are recognized and defined on

1120-464: The Earth's surface by volcanoes, and in layered intrusions formed deep underground. Igneous layers are generally devoid of fossils and represent magmatic or volcanic activity that occurred during the geologic history of an area. There are a number of principles that are used to explain relationships between strata. When an igneous rock cuts across a formation of sedimentary rock, then we can say that

1176-594: The Granitz, but there are many cycle and footpaths. Local transport and access to the area is provided by the Rügen Light Railway and Binz Seaside Railway ( Binzer Bäderbahn ). On the highest point, the Tempelberg ( 107 m above  sea level (NN) ), Prince Wilhelm Malte I of Putbus had the Granitz hunting lodge constructed in the 19th century. Other landmarks include Granitz House ,

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1232-542: The Quatzendorf sub-plant. About 8,000 of these are retailed each year. Contrary to what the name "writing chalk" (see above ), still used in lithostratigraphy today, suggests, the Rügen chalk is not and was not used for the production of school and wall panel chalk. At least in Central Europe, it is made exclusively of gypsum. With the advent of the wellness and alternative medicine movements, Rügen chalk

1288-510: The basis of observable physical rock characteristics. The lithology of a unit includes characteristics such as chemical and mineralogical composition, texture, color, primary depositional structures , fossils regarded as rock-forming particles, or other organic materials such as coal or kerogen . The taxonomy of fossils is not a valid lithological basis for defining a lithostratigraphic unit. The descriptions of strata based on physical appearance define facies . The formal description of

1344-463: The beginning of the 19th century. Chalk is currently being mined in the Promoisel open pit mine. By 1720, chalk was used in the Granitz for the production of quicklime (CaO) in quarries . However, the foundation for the Rügen chalk industry was not laid until the first half of the 19th century. It was laid by the entrepreneur and naturalist Friedrich von Hagenow (1797-1865). In 1832 he leased

1400-566: The carbon dioxide escapes into the atmosphere, the gypsum is reused in the construction industry. Even before 1945, chalk was shipped by train to Berlin , Bremen , Hamburg , to Ruhrgebiet , to Breslau and Stettin , where it was used in the electrical, paint and cosmetics industries. From the 1960s onwards, in contrast to pre-war production, the VEB Kreidewerk Rügen was supplied with chalk in three grain types as desired – "Malkreide 60", "Feinkreide 40" and "Mikrotherm 20". Under

1456-557: The chalk quarries in the Stubnitz , and in the same year he opened a chalk factory in Greifswald . At that time, the raw chalk came by ship from Jasmund to Hagenow's factory. By slurrying, the raw chalk was separated from the undesirable rock components such as flint (firestones, see above ) and finer-grained impurities (so-called Grand ), and the same principle is still used today. In the days of Hagenows and also long after, however,

1512-504: The company was renamed "VEB Kreidewerk Rügen". During the GDR era, the company belonged to various institutions. It was temporarily subordinate to the Rat des Bezirkes  [ de ] (District Council) Rostock , then belonged to the Association of VEB Bindebaustoffe Halle and then to the "VVB Zement Dessau ", which was later renamed "VEB Zementkombinat Dessau" (ZEKOM). In 1984

1568-455: The dry season of about four weeks. With a residual moisture of approximately 5%, the chalk was ready for shipping at that time. From the turn of the 19th to the 20th century, the mining and processing of the chalk became increasingly industrialized, which significantly increased the production volume of raw chalk and the prepared chalk (known in German as Schlämmkreide .) Even before 1945, about

1624-633: The economic upheavals following the Peaceful Revolution in 1989 and 1990, VEB Zementwerke Rüdersdorf was taken over by Readymix AG and the chalk factory in Klementelvitz was spun off, converted into a GmbH and initially remained with the Treuhandanstalt . The operation of the mine railways for the transport of raw chalk from the Wittenfelde open pit mine north of Klementelvitz, the only active chalk pit on Rügen at that time,

1680-459: The end of the 1990s, the Wittenfelde open pit mine was shut down and in its place the Promoisel open pit mine about 1 km further west was put into operation. At the start of mining, around 25 million t of raw chalk was available there. The freshly broken chalk now reaches the factory via a 2 km long conveyor system, where it is processed into refined chalk in different grain sizes using

1736-474: The excavation and preparation of the chalk were carried out almost exclusively with human muscle power and the work was physically very strenuous. During the late 19th century, the fishing village of Sassnitz, located in the immediate vicinity of the Stubnitz, slowly developed into a centre of the chalk industry, not least because most of the chalk pits were on the Jasmund. A fierce competition developed between

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1792-539: The flint stones were formed, originally came from single-celled plankton ( radiolarians , diatoms ), which lived together with the calcareous algae in the Chalk seas. After the deposition of the coccolith sludge containing radiolaria and diatoms, the SiO 2 of the diatoms dissolved in the water that circulated in the pore space of the sediment and was again precipitated elsewhere in the sediment. These deposits are seen today as

1848-404: The flint stones. Since the flint is clearly more weathering - and erosion-resistant than the limestone, it collects on the beach of the chalk cliff and is transported to neighboring areas of the coast by waves and currents during storms and deposited there. The Feuersteinfelder at Prora are particularly well-known in this regard. There are extensive chalk deposits in the northeastern part of

1904-476: The flow rate and at the same time to guarantee a consistent quality of the chalk with a residual moisture of about 0.5% and grain sizes not above 63 microns, new technologies were developed and a new chalk plant constructed in Klementelvitz after 1958 for 30 million Mark (DDR) . In this context, the heavy physical work in the mine face was completely replaced by modern conveyors such as the excavator UB 80,

1960-429: The form of the Rügen chalk. Another characteristic feature of the Rügen chalk is its high content of flint concretions . These are usually formed as nodules and enriched in individual horizons. Sometimes there are also flat formations of different thicknesses. Particularly large, cylindrical flint concretions are known as "Sassnitz flower pots" (see also →  Paramoudra ). The silicon dioxide (SiO 2 ), from which

2016-410: The formal terms lithodeme , which is comparable to a formation; a suite , which is analogous to a group, and a supersuite , similar to a supergroup. A lithodeme is the fundamental unit and should possess distinctive and consistent lithological features, comprising a single rock type or a mixture of two or more types that distinguishes the unit from those around it. As with formations, a lithodemic unit

2072-407: The geological record). The surface strata resulting is called a conformity . Two types of contact between conformable strata: abrupt contacts (directly separate beds of distinctly different lithology, minor depositional break, called diastems ) and gradational contact (gradual change in deposition, mixing zone). Unconformable : period of erosion/non-deposition. The surface stratum resulting

2128-678: The grave site of Finnish warriors and the Cross Oak ( Kreuzeiche ). The name is probably of Slavic origin and comes from the personal name, Granza , used by the Rani tribe, which first appears as a prince's name in the Saxo Grammaticus in 1168. In 1888, the Waldhalle , a tourist restaurant, was built on the hill of Falkenberg on the clifftop path from Binz to Sellin near the coast. The building had to be abandoned and demolished in

2184-417: The igneous intrusion is younger than the sedimentary rock. The principle of superposition states that a sedimentary rock layer in a tectonically undisturbed stratum is younger than the one beneath and older than the one above it. The principle of original horizontality states that the deposition of sediments occurs as essentially horizontal beds. The principles of lithostratigraphy were first established by

2240-604: The individual chalk plants. Von Hagenow had to give up his business in 1850. As a result, 17 companies with 23 chalk plants merged in 1899 to form a cartel and set up limits on all member's production volumes and prices. In 1928, around 500,000 tonnes of rough chalk from the Jasmunder fractures were mined in Martinshafen at Großer Jasmunder Bodden and loaded in Sassnitz. With 80,000 tonnes of capacity, however,

2296-490: The island of Rügen, on the peninsula of Jasmund . The best known are probably the "Rügener chalk cliffs" of the cliffed coast in the vicinity of Sassnitz (see also →  Stubbenkammer , →  Königsstuhl ). These coastal formations are part of the Jasmund National Park and are under strict nature protection. In the hinterland of the Jasmund, chalk is also found under a 1 to 10 m thick overburden in

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2352-456: The legal independence of the VEB Kreidewerk Rügen was finally abolished and it was assigned to the "VEB Zementwerke Rüdersdorf " as "Operating Part 6". Under favorable conditions, the Klementelvitz chalk works, which after commissioning was considered to be one of the most modern chalk works in Europe, achieved an annual production of 185,000 t chalk and 55,000 t Grand. In the course of

2408-419: The mines, after the tracks had been converted accordingly. Depending on the ground conditions, heavy trucks also took over the removal of debris, and special excavators were used for the installation of preassembled tracks. The chalk was also partially preprocessed in open-cast mining using a "mobile sludge device". Like any other nearly pure limestone, the Rügen chalk can be used for both cement production and

2464-733: The mud chalk production on the Jasmund played only a minor role at that time. The buyers of the raw chalk were mainly the Portland cement plants in Wolgast , Lebbin and Stettin . So some pits and chalk plants on the Jasmund belonged directly to the Stettiner Portlandzementfabrik A. G. of Martin Quistorp . The other major chalk and cement producer and most important player in the Rügen Chalk Cartel

2520-471: The name "Three Crown Chalk" (trade name of the Swedish Pomeranian era), this was a major export item of the GDR, which was delivered to 40 countries. Customers continued to include the rubber and cable industry and plants in the paint and paint industry, as well as the cosmetics and pharmaceutical industries. Since 1974, powdered chalk has been processed as a white pigment for the paint "GW 12" in

2576-410: The new wet processing technology. The annual production of the plant is now up to 500,000 t. In 2009 the planning approval was issued for the future Goldberg / Lancken-Dubnitz mining field south of Klementelvitz for production through 2117 of 35 million t of chalk. In the 19th and early 20th century, the chalk had to be dislodged from a steep mine face with pickaxes and transported on lorries to

2632-468: The northern line from Gummanz. The Rügen Kleinbahn also played an important role in transport to the ports. In 1914, in order to relieve the ports of Sassnitz and Martinshafen, Wiek on the Wittow completed the so-called Kreidebrücke for loading the chalk on barges, which was reopened 100 years later as a "floating promenade". Production continued after 1945 with pre-war technology. In order to increase

2688-402: The production of agricultural lime . A relatively modern field of application of limestone is flue-gas desulfurization , and Rügen chalk of inferior quality is put to this use, especially in the coal power plants , Rostock Power Station and Jänschwalde Power Station . Sulfur oxides (SO X ) react with the calcium carbonate to produce gypsum (CaSO 4 ) and carbon dioxide (CO 2 ). While

2744-457: The quality of correlation is improving, but meanwhile the wrong geological decisions could be made that increases the expenses of geological projects. The law of superposition is inapplicable to intrusive, highly deformed, or metamorphic bodies of rock lacking discernible stratification. Such bodies of rock are described as lithodemic and are determined and delimited based on rock characteristics. The 1983 North American Stratigraphic Code adopted

2800-420: The rock was formed. Sedimentary layers are laid down by deposition of sediment associated with weathering processes, decaying organic matter (biogenic) or through chemical precipitation. These layers are often distinguishable as having many fossils and are important for the study of biostratigraphy . Igneous layers occur as stacks of lava flows, layers of lava fragments (called tephra ) both erupted onto

2856-474: The same geological body now (or belonged in the past). The identification is based on comparison of physical and mineralogical characteristics of the rocks, and on general assumptions known as the Steno's principles: 1. The sedimentary strata occurred sequentially in time: the youngest at the top. 2. The strata are originally horizontal. 3. The stratum extends in all directions until it thins out or encounters

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2912-402: The settling basin, in which the still- suspended particles settled out and accumulated into a layer about 30 cm thick. The now no longer cloudy water was drained and the basin was filled with fresh chalk suspension, so that the fine particles could settle again. The whole process was repeated until the sediment reached a thickness of approximately 1.5 meters. The finished fine chalk still had

2968-465: The so-called agitators . In large vats, in which iron hooks rotated, the chalk was stirred with the addition of water. In this step, the coarsest components, mostly flint, were separated. The chalk and water mixture, also called Kreidemilch or Kreidetrübe , was passed through separation tanks where the finer impurities, the Grand , settled out. The chalk suspension freed from the grand finally ended up in

3024-416: The subsoil. There are many quarries and open pit mines, almost all of which have since been abandoned due to inefficiency or for reasons of landscape protection. Overflowing with water, they can be seen in aerial photos of Jasmund as small and large lakes and ponds (the currently largest is the “Kreidesee Wittenfelde”). Even in the urban area of Sassnitz one can still see old chalk quarries, but they date from

3080-630: Was discontinued. On August 13, 1993, after clarification of all land ownership issues, the Kreidewerk Rügen GmbH was taken over by the Vereinigte Kreidewerke Dammann KG and thus the Swiss Omya AG . By then, the company's sales had fallen to only 25,000 t. Omya invested in total by 2010 almost €50 million and built a state-of-the-art facility for chalk production - from excavation to loading. At

3136-610: Was the Pommersche Industrieverein a. A. founded in 1872 by Johannes Quistorp . With the collapse at the end of the Second World War, chalk extraction and processing came to a temporary standstill. Some facilities, including the chalk cable car to Sassnitz harbor, were dismantled and brought to the Soviet Union as war reparations . In addition, the fact that the island of Rügen belonged to

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