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Journal articles on the topic 'Harz (Germany)'

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Published: 26 July 2024
Last updated: 27 July 2024

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1

Cook, Robert B. "Connoisseur's Choice: Manganite Ilfeld, Harz, Germany." Rocks & Minerals 74, no. 4 (January 1999): 250–52. http://dx.doi.org/10.1080/00357529909602547.

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2

Lüders, Volker, and Peter Möller. "Fluid evolution and ore deposition in the Harz Mountains (Germany)." European Journal of Mineralogy 4, no. 5 (October 14, 1992): 1053–68. http://dx.doi.org/10.1127/ejm/4/5/1053.

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3

Hauck, Markus. "New and notable lichens from the Harz Mountains (Northern Germany)." Herzogia 11 (December 20, 1995): 219–23. http://dx.doi.org/10.1127/herzogia/11/1995/219.

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4

Henningsen, Dierk. "The Graywackes of the western part of the Tanne Zone (Harz, Germany)." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1991, no. 5 (June 18, 1991): 284–90. http://dx.doi.org/10.1127/njgpm/1991/1991/284.

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5

Disney, R. Henry L. "Two new species of Phora Latreille (Diptera: Phoridae) from Germany." Entomologist's Gazette 71, no. 2 (April 24, 2020): 130–34. http://dx.doi.org/10.31184/g00138894.712.1761.

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6

Becker, Thomas, and Hartmut Dierschke. "Vegetation response to high concentrations of heavy metals in the Harz Mountains, Germany." Phytocoenologia 38, no. 4 (January 21, 2009): 255–65. http://dx.doi.org/10.1127/0340-269x/2008/0038-0255.

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7

Paul, J., and T. M. Peryt. "Kalkowsky's stromatolites revisited (Lower Triassic Buntsandstein, Harz Mountains, Germany)." Palaeogeography, Palaeoclimatology, Palaeoecology 161, no. 3-4 (September 2000): 435–58. http://dx.doi.org/10.1016/s0031-0182(00)00098-5.

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8

Brink, Heinz-Jürgen. "Die Struktur der Kruste von Harz und Umgebung: Übersicht und Analyse." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 162, no. 3 (September 1, 2011): 235–50. http://dx.doi.org/10.1127/1860-1804/2011/0162-0235.

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9

Klisch, I., and R. G. Gevorkyan. "Regularity of rocks granitization process of massif Brocken (Harz, Germany)." Vestnik Otdelenia nauk o Zemle RAN 3, Special Issue (June 17, 2011): 1–7. http://dx.doi.org/10.2205/2011nz000165.

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10

Bozau, Elke, Hans-Joachim Stärk, and Gerhard Strauch. "Hydrogeochemical characteristics of spring water in the Harz Mountains, Germany." Geochemistry 73, no. 3 (October 2013): 283–92. http://dx.doi.org/10.1016/j.chemer.2013.02.002.

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11

Bozau, Elke, Tobias Licha, and Wilfried Ließmann. "Hydrogeochemical characteristics of mine water in the Harz Mountains, Germany." Geochemistry 77, no. 4 (December 2017): 614–24. http://dx.doi.org/10.1016/j.chemer.2017.10.001.

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12

Herrmann, A., and D. Duncker. "Runoff formation in a tile-drained agricultural basin of the Harz Mountain Foreland, Northern Germany." Soil and Water Research 3, No. 3 (October 31, 2008): 83–97. http://dx.doi.org/10.17221/20/2008-swr.

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By taking two different tile-drained agricultural basins with porous aquifers in the lowlands of northern Germany as examples, it is demonstrated with an integrated study approach that this type of basin responds similarly to an input as forested mountainous basins with dominant fractured rock aquifers in the central European highlands do. The control mechanism is local rise of pressure heads of aquifers starting with the infiltration process. It is shown that drain laterals in agricultural basins function like fractures and faults in those hard rock basins, i.e. as efficient drain pipe lines. This effect is amplified by hydraulic pressure transmission in the course of single input events, and additionally verified here with the help of artificial and environmental tracers. As a result stream flow is predominantly generated by exfiltrating groundwater. For this process drain laterals constitute fast hydraulic short cuts in the sense of preferential flow paths preferably in case that groundwater tables reach up to the level tile-drain networks.
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13

Fritsch, R. "Cytological studies on bryophytes frmo the Harz Mtns, Germany. III. Chromosome counts of mosses." Herzogia 7, no. 3-4 (June 30, 1987): 459–83. http://dx.doi.org/10.1127/herzogia/7/1987/459.

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14

Moraiti, E., B. Christaras, and R. Brauer. "LANDSLIDE IN NACHTERSTEDT OF GERMANY." Bulletin of the Geological Society of Greece 43, no. 3 (January 24, 2017): 1267. http://dx.doi.org/10.12681/bgsg.11303.

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On July 18, 2009, an important landslide occurred in Nachterstedt City toward to the artificial Concordia Lake, which was created, in 1994, at the place of an old coal mine, at the edge of the city. The area is located to North-East of Harz, between the cities of Aschersleben and Quedlingburg. An underground coal mine is responsible for this damage which caused the damage of a privet house and a big building. Three people were also died. The mine apparently closed in 1991 whereupon it was converted into a recreation area. The landslide was caused by the increase of the groundwater level, in the coal mine, after a heavy rain, in relation to the water level of the lake.
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15

Bock, Jan-Jonathan. "Migrants in the Mountains: Shifting Borders and Contested Crisis Experiences in Rural Germany." Sociology 52, no. 3 (June 2018): 569–86. http://dx.doi.org/10.1177/0038038518759459.

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When one million asylum seekers and other migrants entered Germany in 2015–2016, the situation was called a national crisis. This article examines the impact of an emergency reception centre on a small town, investigating how rural Germans debated crisis experiences, migration and borders. In the Harz Mountains, asylum seekers arrived in an area already suffering from decline. Accommodating newcomers became a specific challenge. The assumption of a European-wide emergency induced by the presence of foreigners neglects how contexts shape crisis perceptions. Social fragmentation occurred when some townspeople framed local developments as the Flüchtlingskrise covered by the media, whereas others used personal experience to critique the crisis concept. As new experts in emergency management, reception centre employees changed their political consciousness. The unsteady politico-spatial order, rather than asylum seekers as subjects, produced anxiety over marginalisation, since the reception centre shifted problematic border features – chaos and risk – into central Germany.
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16

Lehmann, Lisa, and Clara Stefen. "Study of non-metric characters of the skull to determine the epigenetic variability in populations of the European wildcat (Felis silvestris silvestris) and domestic cats (Felis catus)." Mammalian Biology 101, no. 4 (April 16, 2021): 407–17. http://dx.doi.org/10.1007/s42991-021-00119-0.

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AbstractWe studied the variability of non-metric cranial traits, mainly foramina, of European wildcats (Felis silvestris silvestris) and domestic cats (Felis catus) from Germany based on 28 non-metric traits in 211 skulls. The domestic cats were grouped together as a statistical population. The wildcats were divided into two populations: Harz and Hesse, which were further subdivided, based on traffic infrastructure, natural landscape, and in the Harz, on time period. Epigenetic variability, epigenetic distance and the fluctuating asymmetry were calculated to assess genetic variability, possible depressions and population stability. The epigenetic variability Iev of the wildcat groups ranged from 0.27 (Hesse II) to 0.40 (Harz I). The difference in Iev between all specimens from Harz and Hesse respectively was less (Iev = 0.37 Harz and 0.31 Hesse). Compared to other studies these values are not assumed to indicate genetic depression. The epigenetic distance between the wildcat samples is 0.0774 overall, and in each case higher between sub-groups of the Harz and Hesse than between groups within these regions, respectively. The significant epigenetic distance between Harz and Hesse might indicate—at least past formerly—restricted connectivity between these regions. The fluctuating asymmetry for wildcats in total is 11.74% and in the sub-groups it ranges from 8.47 to 16.14%. These values are below 20% are at the lower range known from populations of other mammal species. The use of fluctuating asymmetry had also been discussed critically in its usefulness to assess viability of populations.
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17

Stanley, C. J., A. J. Criddle, H. J. Forster, and A. C. Roberts. "TISCHENDORFITE, Pd8Hg3Se9, A NEW MINERAL SPECIES FROM TILKERODE, HARZ MOUNTAINS, GERMANY." Canadian Mineralogist 40, no. 2 (April 1, 2002): 739–45. http://dx.doi.org/10.2113/gscanmin.40.2.739.

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18

Kaufmann, Georg, Douchko Romanov, and Ralf Nielbock. "Cave detection using multiple geophysical methods: Unicorn cave, Harz Mountains, Germany." GEOPHYSICS 76, no. 3 (May 2011): B71—B77. http://dx.doi.org/10.1190/1.3560245.

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Unicorn cave in the southern Harz Mountains of Germany is a show cave in dolomitic rocks of the Zechstein Formation. The cave’s trunk passage is interrupted by larger rooms. The overburden is only around 15 m. The passages are filled with sediments that can be up to 50 m thick. We used gravimetry and electrical resistivity imaging over the cave area to identify the subsurface voids and the extent of the sediment infill of the cave passages. Our choice of methods was based on several conditions unique to the cave: (1) well surveyed, (2) shallow overburden, (3) large air-filled passages, and (4) thick sediment cover, concealing true passage size. Using the cave survey as an initial model for the subsurface structure, we successfully identified the air-filled cave with both methods. We then inferred the thickness of the sediment infill by forward modeling and identified a possible southward continuation beyond the currently explored passages.
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19

König, Stefan, and Volker Wrede. "On the Structure of the Borders of the Harz Mountains (Germany)." Zeitschrift der Deutschen Geologischen Gesellschaft 145, no. 1 (January 1, 1994): 153–71. http://dx.doi.org/10.1127/zdgg/145/1994/153.

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20

Bruelheide, Helge, and Thomas Flintrop. "Evaluating the transplantation of a meadow in the Harz Mountains, Germany." Biological Conservation 92, no. 1 (January 2000): 109–20. http://dx.doi.org/10.1016/s0006-3207(99)00061-0.

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21

Kaufmann, Georg, Douchko Romanov, Ralf Nielbock, and Joyce Lundberg. "The sediment record of the Unicorn Cave, southern Harz Mountains, Germany." Geomorphology 367 (October 2020): 107295. http://dx.doi.org/10.1016/j.geomorph.2020.107295.

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22

Führer, F. X. "Geological results of recent geophysical investigations in the Harz Mountains (Germany)." Geologische Rundschau 77, no. 1 (February 1988): 79–99. http://dx.doi.org/10.1007/bf01848677.

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23

Gischler, Eberhard. "Guilds and cycles in Devonian fore reef limestones: a preliminary study (Iberg Reef, Harz Mts., Germany)." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1995, no. 5 (May 1, 1995): 279–94. http://dx.doi.org/10.1127/njgpm/1995/1995/279.

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24

Günther, A., A. Carstensen, and W. Pohl. "Automated sliding susceptibility mapping of rock slopes." Natural Hazards and Earth System Sciences 4, no. 1 (March 9, 2004): 95–102. http://dx.doi.org/10.5194/nhess-4-95-2004.

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Abstract. We present a suite of extensions for ARCVIEW GIS™ (ESRI) that allows to map the spatial distribution of first-order mechanical slope-properties in hard rock terrain, e.g. for large slope areas like water reservoir slopes. Besides digital elevation data, this expert-system includes regional continuous grid-based data on geological structures that might act as potential sliding or cutoff planes for rockslides. The system allows rapid automated mapping of geometrical and kinematical slope properties in hard rock, providing the basis for spatially distributed deterministic sliding-susceptibility evaluations on a pixel base. Changing hydrostatic slope conditions and rock mechanical parameters can be implemented and used for simple predictive static stability calculations. Application is demonstrated for a study area in the Harz Mts., Germany.
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25

Segeritz, Lisa, Ole Anders, Tomma Lilli Middelhoff, Deliah Tamsyn Winterfeld, Pavlo Maksimov, Gereon Schares, Franz Josef Conraths, Anja Taubert, and Carlos Hermosilla. "New Insights into Gastrointestinal and Pulmonary Parasitofauna of Wild Eurasian lynx (Lynx lynx) in the Harz Mountains of Germany." Pathogens 10, no. 12 (December 20, 2021): 1650. http://dx.doi.org/10.3390/pathogens10121650.

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The Eurasian lynx (Lynx lynx) represents an endangered wild felid species. In Germany, it currently occurs in three isolated populations in and around the Harz Mountains, the Palatinate Forest and the Bavarian Forest. Lynx parasitic infections affect animal health and might have an influence on population performance. Therefore, we investigated the protozoan and helminth fauna of free-ranging Eurasian lynx of the Harz population with emphasis on zoonotic parasites. Individual scat samples (n = 24) were collected from wild animals between 2019 and 2021 in the Harz National Park and surrounding areas. In total, 15 taxa of endoparasites were detected, including seven nematodes (i.e., Aelurostrongylus abstrusus, Angiostrongylus spp., Uncinaria stenocephala, Toxascaris leonina, Toxocara cati, Cylicospirura spp. and Capillaria spp.), one cestode (Diphyllobothriidae) and one trematode (Heterophylidae) as well as six protozoans (i.e., Cystoisospora rivolta, Cystoisospora felis, Toxoplasma gondii/Hammondia spp., Sarcocystis spp., Giardia intestinalis and Cryptosporidium spp.). Moreover, first-stage larvae (L1) of spurious lungworm, Protostrongylus pulmonalis, originating from lagomorph preys were identified. This work represents the first report on patent A. abstrusus and Angiostrongylus spp. infections in wild German Eurasian lynxes. Some of the identified parasites represent relevant pathogens for lynxes, circulating between these carnivorous definitive hosts and a variety of mammalian and invertebrate intermediate hosts, e.g., Sarcocystis spp., T. gondii/Hammondia spp., T. cati, T. leonina, A. abstrusus and Angiostrongylus spp., while others are considered exclusively pathogenic for wild felids (e.g., Cylicospirura spp., C. rivolta, C. felis). This study provides insights in the occurrence of zooanthroponotically relevant metazoan (i.e., T. cati and U. stenocephala) and protozoan (i.e., G. intestinalis) species in free-ranging lynx. The present work should be considered as a baseline study for future monitoring surveys on endoparasites circulating in wild Eurasian lynx for appropriate management practices in lynx conservation strategies in Europe.
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26

Röhling, Heinz-Gerd, Ralf Nielbock, Georg Kaufmann, David Colin Tanner, Jan Igel, Ulrich Polom, Henning Zellmer, and Detlef Vogel. "An integrated geophysical and geological interpretation of the area around the Unicorn Cave (Southern Harz Mountains, Germany)." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 170, no. 2 (December 9, 2019): 117–44. http://dx.doi.org/10.1127/zdgg/2019/0195.

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27

Ma, Chi, Hans-Jürgen Förster, and Günter Grundmann. "Tilkerodeite, Pd2HgSe3, a New Platinum-Group Mineral from Tilkerode, Harz Mountains, Germany." Crystals 10, no. 8 (August 8, 2020): 687. http://dx.doi.org/10.3390/cryst10080687.

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Tilkerodeite, ideally Pd2HgSe3, is a new platinum-group selenide from the Eskaborner Stollen (Adit Eskaborn) at Tilkerode, Harz Mountains, Germany. Tilkerodeite crystals occur as euhedral inclusions in tiemannite or as extremely fine-grained lamellar aggregates (grain-size up to 3 μm) in a dolomite–ankerite matrix, together with clausthalite, tiemannite, jacutingaite, stibiopalladinite, and native gold. Neighbouring Se-bearing minerals include tischendorfite and chrisstanleyite. Tilkerodeite is opaque with a metallic luster, and is flexible in blade-like crystals, with perfect basal cleavage {001}. In plane-polarized light, tilkerodeite is brownish-grey. It is weakly bireflectant, and weakly pleochroic in shades of light-brown and grey. The anisotropy is weak, with rotation tints in weak shades of greenish-brown and grey-brown. The range of reflectance is estimated in comparison to clausthalite with 45–50%. Electron-microprobe analyses yield the mean composition (wt. %) Se 32.68, Hg 26.33, Pt 20.62, Pd 15.89, Pb 2.72, Cu 0.66, S 0.27, total 99.17 wt. %. The empirical formula (based on six atoms pfu) is (Pd1.08Pt0.76Pb0.09Cu0.07)Σ2.00Hg0.95(Se2.98S0.07)Σ3.05. The ideal formula is Pd2HgSe3. Tilkerodeite is trigonal, with Pt4Tl2Te6-type structure, space group P3–m1, a = 7.325(9) Å, c = 5.288(6) Å, V = 245.7(9) Å3, and Z = 2. It is the Pd-analogue of jacutingaite. Tilkerodeite formed hydrothermally, possibly involving the alteration of tiemannite by low-temperature oxidizing fluids. The new species has been approved by the IMA-CNMNC (2019-111) and is named after the locality. Tilkerode is the most important selenide-bearing occurrence in Germany and type locality of naumannite, eskebornite, and tischendorfite.
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28

de Oliveira Pinto, Tiago. "Songbird and birdsong: Listening to the finches in the Harz region, Germany." Sound Studies 6, no. 2 (July 2, 2020): 215–38. http://dx.doi.org/10.1080/20551940.2020.1799543.

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29

Lükewille, Anke, and Jürgen Prenzel. "Reconstruction of water acidification in a forested catchment, western Harz Mountains, Germany." Applied Geochemistry 8 (January 1993): 131–34. http://dx.doi.org/10.1016/s0883-2927(09)80024-3.

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30

Kaufmann, Georg, and Douchko Romanov. "Geophysical investigation of a sinkhole in the northern Harz foreland (North Germany)." Environmental Geology 58, no. 2 (October 28, 2008): 401–5. http://dx.doi.org/10.1007/s00254-008-1598-0.

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31

Langheinrich, Uta, Dirk Böhme, Uwe Wegener, and Volker Lüderitz. "Streams in the Harz National Parks (Germany) — a hydrochemical and hydrobiological evaluation." Limnologica 32, no. 4 (December 2002): 309–21. http://dx.doi.org/10.1016/s0075-9511(02)80022-6.

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32

Rinke, Karsten, Burkhard Kuehn, Serghei Bocaniov, Katrin Wendt-Potthoff, Olaf Büttner, Jörg Tittel, Martin Schultze, et al. "Reservoirs as sentinels of catchments: the Rappbode Reservoir Observatory (Harz Mountains, Germany)." Environmental Earth Sciences 69, no. 2 (April 12, 2013): 523–36. http://dx.doi.org/10.1007/s12665-013-2464-2.

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33

Round, F. E., and H. Håkansson. "CYCLOTELLOID SPECIES FROM A DIATOMITE IN THE HARZ MOUNTAINS, GERMANY, INCLUDINGPLIOCAENICUSGEN. NOV." Diatom Research 7, no. 1 (May 1992): 109–25. http://dx.doi.org/10.1080/0269249x.1992.9705202.

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34

Baumann, Albrecht, Borwin Grauert, Sabine Mecklenburg, and Roland Vinx. "Isotopic age determinations of crystalline rocks of the Upper Harz Mountains, Germany." Geologische Rundschau 80, no. 3 (October 1991): 669–90. http://dx.doi.org/10.1007/bf01803694.

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35

Haude, Reimund. "A rare Palaeozoic echinoid from the terminal phase of the Iberg Atoll (Frasnian, Harz Mts., Germany)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 214, no. 1-2 (November 10, 1999): 149–67. http://dx.doi.org/10.1127/njgpa/214/1999/149.

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36

SCHMULL, Michaela, and Markus HAUCK. "Lecidea hercynica, a new montane epiphytic lichen from Germany." Lichenologist 37, no. 6 (October 27, 2005): 485–89. http://dx.doi.org/10.1017/s0024282905015422.

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Lecidea hercynica Hauck & Schmull is described as a new species from Germany. It is characterized by a poorly developed or bullate to verrucose, areolate thallus on whitened spots of the substratum, numerous plane to yellowish brown to black, convex apothecia with a persistent margin, Micarea type-like asci, and by the presence of atranorin and protocetraric acid. It does not belong to Lecidea s. str., but is provisionally placed in Lecidea s. lat. until a taxonomic treatment of the whole group has been carried out. Lecidea hercynica is widespread in high-elevation forests of Picea abies in the Harz Mountains, where it grows preferably on decorticated wood in open situations.
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37

이덕재. "Affective Appraisal on Natural Landscapes by Visitors to Harz National Park of Germany." Journal of Korean institute of Forest Recreation 21, no. 1 (March 2017): 59–68. http://dx.doi.org/10.34272/forest.2017.21.1.006.

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38

Gereke, Manfred, Friedrich Wilhelm Luppold, Matthias Piecha, Eberhard Schindler, and Dieter Stoppel. "The type locality of the Kellwasser-Horizons in the Upper Harz Mountains, Germany." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 165, no. 2 (June 1, 2014): 145–62. http://dx.doi.org/10.1127/1860-1804/2014/0066.

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39

Ruppert, H., and M. Deicke. "Source of medieval lead enrichments in natural archives of Europe: Harz Mts. (Germany)." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A545. http://dx.doi.org/10.1016/j.gca.2006.06.1006.

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40

GANSSLOSER, MARTIN. "Detrital chromian spinels in Rhenohercynian greywackes and sandstones (Givetian–Visean, Variscides, Germany) as indicators of ultramafic source rocks." Geological Magazine 136, no. 4 (July 1999): 437–51. http://dx.doi.org/10.1017/s0016756899002770.

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More than 75% of heavy mineral spectra of Rhenohercynian greywackes from the Harz Mountains (Famennian–Visean), the Werra greywacke (Frasnian–Famennian) and the Rhenish Slate Mountains (Frasnian–Visean) contain small amounts of detrital chromian spinels. Similar grains have also been proven in sandstones of the Givetian Stiege beds (East Harz nappe). These sandstones are derived from the area of the Mid German Crystalline Rise, which is commonly interpreted as the source area of the Rhenohercynian greywackes. Microprobe analyses have revealed mainly a picotite composition. Presumable source rocks were chiefly Alpine-type peridotites. Due to the onset of spinel sedimentation in Givetian times, these peridotites must be at least partly of pre-Givetian age, and are assumed to be linked to Cadomian subduction. Potential source rocks are not exposed in the present outcrops of the Mid German Crystalline Rise nor in the Rhenohercynian zone or the Northern Phyllite zone, which implies that the presumed mafic to ultramafic lithologies were completely eroded and/or downfaulted during later stages of the Variscan orogeny.
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41

Diercks, Manuel-L., Klaus Stanek, Leomaris Domínguez-Gonzalez, and Bodo Ehling. "Quaternary landscape evolution and tectonics in Central Germany – A case study of the Harz." Geomorphology 388 (September 2021): 107794. http://dx.doi.org/10.1016/j.geomorph.2021.107794.

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42

Bley, K. A. "Floristic and ecological studies of mosses in running waters of the Harz Mtns, Germany." Herzogia 7, no. 3-4 (June 30, 1987): 623–47. http://dx.doi.org/10.1127/herzogia/7/1987/623.

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43

Evers, Christiane. "The Festuco-Brometea-communities north of the Harz Mountains in Lower Saxony, Northwest-Germany." Phytocoenologia 27, no. 2 (June 23, 1997): 161–211. http://dx.doi.org/10.1127/phyto/27/1997/161.

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44

Peckmann, Jörn, Eberhard Gischler, Wolfgang Oschmann, and Joachim Reitner. "An Early Carboniferous seep community and hydrocarbon-derived carbonates from the Harz Mountains, Germany." Geology 29, no. 3 (2001): 271. http://dx.doi.org/10.1130/0091-7613(2001)029<0271:aecsca>2.0.co;2.

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45

Watanabe, Makiko, Shunpei Ohishi, Angelika Pott, Ulrike Hardenbicker, Kumiko Aoki, Nobuo Sakagami, Hiroyuki Ohta, and Nobuhide Fujitake. "Soil chemical properties and distribution of sclerotium grains in forest soils, Harz Mts., Germany." Soil Science and Plant Nutrition 50, no. 6 (February 2004): 863–70. http://dx.doi.org/10.1080/00380768.2004.10408547.

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BRAMBILLA, E., O. PAUKER, S. COUSIN, U. STEINER, A. REIMER, and E. STACKEBRANDT. "High phylogenetic diversity of Flavobacterium spp. isolated from a hardwater creek, Harz Mountains, Germany." Organisms Diversity & Evolution 7, no. 2 (August 2, 2007): 145–54. http://dx.doi.org/10.1016/j.ode.2006.03.003.

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Gischler, Eberhard, and M. Mesut Erkoç. "Facies of Devonian fore reef limestones: a quantitative study (Iberg Reef, Harz Mts., Germany)." Palaeobiodiversity and Palaeoenvironments 93, no. 1 (October 25, 2012): 91–101. http://dx.doi.org/10.1007/s12549-012-0108-2.

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Mottequin, Bernard, and Dieter Weyer. "On some Mississippian (Carboniferous) brachiopods from neptunian dykes of the Harz Mountains (central Germany)." Palaeobiodiversity and Palaeoenvironments 99, no. 3 (February 8, 2019): 447–75. http://dx.doi.org/10.1007/s12549-018-0360-1.

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Vymazalová, Anna, Alexandre R. Cabral, František Laufek, Wilfried Ließmann, Chris J. Stanley, and Bernd Lehmann. "Roterbärite, PdCuBiSe3, a new mineral species from the Roter Bär mine, Harz Mountains, Germany." Mineralogy and Petrology 114, no. 5 (June 4, 2020): 443–51. http://dx.doi.org/10.1007/s00710-020-00703-1.

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L�kewille, Anke, Volker Malessa, and Christine Alewell. "Measured and modelled retention of inorganic sulfur in soils and subsoils (Harz Mountains, Germany)." Water, Air, & Soil Pollution 85, no. 2 (1995): 683–88. http://dx.doi.org/10.1007/bf00476908.

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