Editor C. Petreas Athens, Greece, 4648. Based on morphological and metrical characteristics, all bear remains from LCC are attributed to cave bear (U. spelaeus), making this species the only mammalian taxon identified within the analyzed faunal assemblage from Pleistocene deposits. Freiberg: Technische Universitt Bergakademie Freiberg. Three sets of fractures were recorded within the channel, which significantly influence its shape and formation. Could there be an actual connection between local electromagnetic fields, technology malfunctions, the interest of shadowy organizations in the cave and the alleged paranormal activity taking place? Although most of the remains could not be aged precisely, information of the relative age at death shows predominance of adult bears (81.7%), while the rest belongs to juveniles (Figure 8). In sample DC-SP 7 palynofacies is still dominated by the opaque phytoclasts, mostly corroded charcoal. During the 19th century, the cave also gained notoriety. The authors are thankful to the archaeological firm Kaducej Ltd. which conducted rescue archaeological excavation at LCC, from March to May 2019. 96% of travelers recommend this experience. In the investigated sediment, it was not possible to recognize this carbonate source area, except within the clearly in situ formed Bd facies which contains angular boulders of the host rock (Figure 11A). At the head of the valley in Yosemite National Park - as if on a pedestal - stands Half Dome. doi:10.2475/ajs.248.1.55. 458, 193219. 65 (1), 3241. Cerovake PeineNajvee U Hrvatskoj [Cerovake Caves - the Largest in Croatia - in Croatian]. The myth says that the cave was the hideout of the infamous brigand, Davelis. (2017). Van Geel, B. Inventory of Sedimentary Organic Matter in Modern Wetland (Marais Vernier, Normandy, France) as Source-Indicative Tools to Study Holocene Alluvial Deposits (Lower Seine Valley, France). After decades of searching, investigators seem no closer to finding the answer than they were in the 1960s. Oltenia. Dinaric Karst-Geography and Geology, in Chapter 40 - Dinaric KarstGeography and Geology in Encyclopedia of Caves. The buildings of our Nation's Capital are constructed with rocks from quarries located throughout the United States and many distant lands. doi:10.1111/j.1475-4754.1979.tb00241.x. Sedimentary facies analysis coupled with the palynofacies analysis revealed changes in depositional events within the LCC, ranging from intensive collapse processes with fluvial influence through re-deposition by mechanisms of high density flows to the forming of stagnant water environments with laminated sediments, and finally to the terrestrial environment with pronounced human activity. It is evidenced with similar facies types (Sw) of detrital sediments which were found within the hypsometrically highest horizontal level of the todays CCS (Talaja and Kurei, 2017). At Postojnska Cave, the sequence follows the series of events: formation of the fault, growth of the initial conduit due to groundwater circulation through the fault, infilling of the conduit with allogenic sediment, abandonment due to regional base level lowering, and continued motion along the fault (Sasowsky et al., 2003). All bone and teeth fragments were carefully examined with a hand lens (10 magnification) looking for any bone modifications that could indicate butchery, gnawing, and other taphonomic traces as direct indicators of different agencies responsible for the accumulation and preservation of the skeletal material. Share sensitive information only on official, secure websites. To conclude, the mineral composition of the clastic detritus in which there is high proportion of quartz, followed by feldspars, muscovite, opaque minerals, biotite, chlorite, chromite, pyroxenes, zircon, rutile, garnets, epidote, zoisite/clinozoisite group minerals and chromite can indicate a diverse source area, but the one that is geographically connected to the nearby river Otua catchment area. His interests include planetary geology, astrobiology, paleontology, archaeology, history, space archaeology, and SETI. 32, 523528. Krina Jama (SW Slovenia): Numerical-And Correlated-Ages from Cave bear-bearing Sediments. Although it is a new approach in the region, the application of luminescence dating techniques has proven to be a suitable chronometer in cave settings (e.g., Montanari et al., 2019). White, E. L. (2019). tiinele Naturii. The ancient church and natural cave networks had been severely damaged. Hence, it is possible that beside the tiny bone fragments in the fine-grained part of the sample DC-SP 1, a part of the HA may also have originated from the in situ bat guano, as indicated by the dark color of the sediment. (2019). The increase of 14C activity of dissolved inorganic carbon along the river course. Caleb Strom is currently a graduate student studying planetary science. During early Christianity, monks chose to go there for their hermitages, while many isolated themselves in the dank mountain caves. However, a closer examination of the differential representation of different body parts revealed the following: the most abundant class are trunk elements (32.2%), closely followed by the elements of the head (teeth included; 29.1%) and feet bones (25.2%). We assumed in situ genesis of the flowstone because platy fragments (Figures 9AC) are distributed at the same horizontal level with visible distinct uneven base/nucleation plane shoving traces of the underlying silty-clayey sediment (Supplementary Material S2). 3, 7597. Developments in Radiation, Stimulation and Observation Facilities in Luminescence Measurements. In the laboratory the faunal remains were washed and dried and a detailed palaeontological analysis was conducted at the Institute for Quaternary Palaeontology and Geology in Zagreb. Beside kaolinite, vermiculite, illite/muscovite, chlorite and mix-layered clay minerals, samples DC-SP 2 to DC-SP 6 contain minerals from the talc-pyrophillite group (Table 2). Among them, the most common are chert particles. Editor L. Bakari (Zagreb: Archaeological museum Zagreb), 2160. Glad You Asked: What Are Those Blue Ponds Near Moab? 75 (14), 105153. Clastic sedimentary rocks are made up of pieces (clasts) of pre-existing rocks. 157, 372387. 9:672229. doi: 10.3389/feart.2021.672229. Igneous rocks form when molten rock (magma or lava) cools and solidifies. Examples include: breccia, conglomerate, sandstone, siltstone, and shale. This is still not verified as a historical fact, so a lot of people are still looking for his treasure! Third Edition (Boston: Elsevier Academic Press), 353362. The Katholikon, or central church of the monastery, and its nursing home are all that have survived the original monasterial complex. The allogenic cave deposits in Croatia have been poorly explored, especially from the point of view of their origin and depositional mechanisms. Senjski zbornik. Radiocarbon age was rounded of digits in accordance with the recommendations given by Stuiver and Polach (1977). Boreas 38 (2), 189206. This number is based on the percentage of all Tripadvisor reviews for this product that have a bubble rating of 4 or higher. Not to geologists. in press. doi:10.1016/B978-0-12-814124-3.00020-0, White, W. B. Then, two things happened: either Chaos or Gaia created the universe as we know it, or Ouranos and Tethys gave birth to the first beings. Heavy Minerals in Colour. Microscopic charcoal remains (around 100 microns in size; Figure 7B) point to the influence of fire (Whitlock and Larsen, 2002). Latest Earthquakes | Live WebChatShare Social Media. The oldest Byzantine construction to remain standing there is Agios Spyridonas (12th century), a chapel carved into the renowned Davelis Cave . However, even though cave sediments show similarities to Terra Rossa type soils, they cannot be classified as soils (Zupan Hajna et al., 2020). Figure 5.3. Chang, S. J., Blake, R. E., Stout, L. M., and Kim, S. J. Maybe, natural pressure on the semi-marble walls of the cave could occasionaly create some electric field disturance, but this has yet to be proven. [Online] Available at: http://mentalfloss.com/article/70293/6-scientific-explanations-ghostsN.D. Namely, the horizon of the Di facies could be related to deposits earlier described in the caves of the nearby Graac area as sediment composed of reddish-brown phosphate clays with numerous osteological remains of the Late Pleistocene with traces of the Upper Paleolithic culture (Malez, 1960b; Ivanovi et al., 1976). doi:10.1016/j.quaint.2018.05.045, Zupan Hajna, N., Bosk, P., Pruner, P., Mihevc, A., Hercman, H., and Horek, I. Status Report on the Zagreb Radiocarbon LaboratoryAMS and LSC Results of VIRI Intercomparison Samples. 10H2O) against coagulation, cold HCl (15%) and HF (40%), removing carbonates and silica, respectively. What Are Sedimentary Rocks? Conditions like these are found deep within the Earth or where tectonic plates Igneous rocks (from the Latin word for fire) form when hot, molten rock crystallizes and solidifies. 494, 5265. The word mausoleum is nowadays defined as a special building made to hold the dead body of an important person or the deceased bodies of a family. 2018. The appearance of microscopic-sized charcoal remains (Figure 7B) and possible traces of guano and bone remains (Table 2) between collapsed blocks of the Bd facies indicate that during the deposition of the Bd facies the cave channel was already fully developed and well connected to the surface in an open-air environment. - Geoloki vjesnik. Polygenetic, detrital, and residual origins are most commonly mentioned (Durn et al., 2007). Discover my books: bit.ly/elefteriaLet's connect: instagram.com/flowathens/facebook.com/elefteria.flowMusic:Organic Meditation by Kevin MacLeodLink: https://incompetech.filmmusic.io/song/3860-healingLicense: https://filmmusic.io/standard-licenseText resources:Wikipedia and EPOD - a service of USRA. Ancient TL. Chemical Sedimentary Rock: Definition & Examples | Study.com The THM are very sparse in the samples. Among the HMF, the amount of opaque minerals is high, about 90%. Given the chaotic arrangement of clasts and random orientation of long bones with no visible textures in the clayey silt, the facies of the red clayey silt is interpreted as Di facies (e.g., Bosch and White, 2004; White, 2007; Haddad-Martim et al., 2017). Sedimentary rocks are formed by a very long process of erosion and compression. (2020). J. 29 March 2018 View The mysteries of Greece's Davelis Cave have been perplexing locals for years. Hence, it can be assumed that sedimentation of the Bd facies in the channel of the LCC could also happen during a relatively cold period. Sedimentary Rocks Lesson #13 | Volcano World | Oregon State University Res. A thin layer of laminated flowstone composed of columnar sparry calcite was determined with visible crystal growth directions (Supplementary Material S2). The resulting igneous rocks can vary widely in appearance. Tomasaki, Mt. 41, 317328. Beograd: Savezni geoloki institut, 62. Microscopic analyses were performed using the Olympus BH-2 and Leica DM2500 microscope (Croatian geological survey). Ljubljana: Zaloba ZRC, 180. Limestonecan also form by precipitating directly out of the water. Sedimentology and Paleomagnetism of Sediments, Kartchner Caverns, Arizona. 2015. Wood, G. D., Gabriel, A. M., and Lawson, J. C. (1996). Zagreb: Zavod za geologiju. 5.3: Sedimentary Rocks - Geosciences LibreTexts 2, April 1996. doi:10.1016/j.quaint.2014.10.013, PubMed Abstract | CrossRef Full Text | Google Scholar, Bickel, L., Lthgens, C., Lomax, J., and Fiebig, M. (2015b). doi:10.1007/978-1-4419-9118-8_9, Whitlock, C., and Larsen, C. (2002). (2011). Env Geol. doi:10.1016/j.gca.2017.04.038. 6 Scientific Explanations for Ghosts . Chromite grains, slightly reddish-brown colored, are present in all analyzed samples and in some samples pyrite (Figure 5D). Colorless garnets predominate. 420 Exterior of the rare, double-church of the Byzantine age built. The second most common translucent heavy mineral is zircon. The major shift in sedimentation mechanisms between collapse and redeposition processes, and deposition within stagnant water conditions commenced through the period after 19.5 ka from today up to the onset of the Late Bronze Age. Netherlands: PANalytical B.V. Almeo. The Contribution of Cosmic Radiation to the Environmental Dose for Thermoluminescent Dating - Latitude, Altitude and Depth Dependencies. A New Graphite Preparation Line for AMS 14C Dating in the Zagreb Radiocarbon Laboratory. Facies types and age on profile DC-SP in the Lower Cerovaka Cave (A) Facies distribution with indicated sampling spots, (B) detail from upper part of Slackwater facies with indicated sampling spot and luminescence age, (C)14C age with indicated sampling spot within flowstone fragment, (D) detail from diamicton facies with visible larger clasts and bone fragments of Ursus spelaeus with indicated sampling spot and luminescence age [authors of photographs (A) DTP, (B)(D) NB]. Quat. Such interpretation shows a good correlation with the sedimentological data. For laboratory dosing, the system is equipped with a 90Sr/90Y beta source delivering a dose of about 0.1Gy/s. Soc. Marble of the Deseret Limestone and Gardison Formation can be seen in Big Cottonwood Canyon, Salt Lake County. Mining-Geology-Petroleum Bull. [Online] Available at: http://www.vembos.gr/pendeliriddle.htmSwancer, Brent. Croatian Geological Survey (2009). It might have been top U.S. governmental pressures to the Greek government. Their names are based on their clast or grain size. Davelis Cave, or Penteli Cave, as it is more commonly called, is a cave historically hidden by pine forests. Cave Clastic Sediments and Implications for Speleogenesis: New Insights from the Mugnano Cave (Montagnola Senese, Northern Apennines, Italy). Luminescence Dating of Glaciofluvial Deposits Linked to the Penultimate Glaciation in the Eastern Alps. Gneiss:(pronounced nice) Gneiss is a high-grade (high heat and pressure) metamorphic rock in which the foliation results from a layering of different mineral groups, which give this rock a banded look of dark (mica, amphibole, and other iron-magnesium minerals) and light (quartz and feldspar) minerals. #1 of 1 things to do in Penteli. Sedimentary Organic MatterOrganic Facies and Palynofacies. Rare occurrences of biotite and greenish anhedral amphiboles are also present. Common extrusive rocks are basalt, andesite, and rhyolite. The mineral ice is the crystalline form of water (H2O). 494, 1933. doi:10.1016/j.quaint.2011.06.048, Durn, G. (2003). doi:10.1016/j.nimb.2012.01.048. Introducing an R Package for Luminescence Dating Analysis. doi:10.1016/0277-3791(94)90064-7, Trbojevi Vukievi, T., and Babi, K. (2008). The surrounding area was used as a marble quarry by the builders of the Acropolis, and the cave was. Except for a single questionable finding of cut marks (Trbojevi Vukievi and Babi, 2008), no traces of butchering were previously found on cave bear bones from LCC, so it is safe to assume that hominins were not responsible for the accumulation and dispersal of cave bear bones. Davelis Cave ( Greek: ) is a well-known cave in Penteli, a mountain to the north of Athens, Greece . Thus, the upper elements of the fore limbs (scapula, humerus, radius, ulna) and hind limbs (pelvis, femur, tibia, fibula) are represented by only 6.1 and 7.4%, respectively. Quaternary Depositional Facies in Cave Entrances and Their Relation to Landscape Evolution: The Example of Cuvieri Cave, Eastern Brazil. If you book with Tripadvisor, you can cancel up to 24 hours before your tour starts for a full refund. The sample DC-SP 1 additionally contains bone fragments and significant amounts of hydroxyapatite (HA) (Table 2). Sedimentary rocks are formed from pre-existing rocks or pieces of once-living organisms. Where do geodes come from? - Scienceline Their relics are now kept in a shrine. The Utah Geological Survey (UGS) is a division of the Utah Department of Natural Resources. Assoc. Palynofacies from the sample DC-SP 2 is dominated by opaque phytoclasts, mostly corroded charcoal, while non-opaque phytoclasts decreased. 210, 208227. It acquired its current form following interventions made in 1953, transforming the church into a Mount Athos-type triple-conch church. For that reason, single quartz and potassium-rich feldspar grains (usually between 63300m) were extracted from the collected samples. The authors would like to thank the editor (Dr. Aurel Peroiu), and the two reviewers (Dr. Andrea Zerboni, and Dr. Christos Pennos) for their comments. Editors C. Koeberl, and D. M. Bice (New York, NY: Geological Society of America Special Paper), 459470. Strange and Dangerous: What Lies at the Heart of Davelis Cave? doi:10.1007/s00254-002-0727-4, Schmid, S. M., Bernoulli, D., Fgenschuh, B., Matenco, L., Schefer, S., Schuster, R., et al. Davelis Cave in Mount Penteli - A short documentary by Elefteria Palaeoecol. (A) Granulometric analysis by sedimentation method: cumulative granulometric curves, (B) distribution curves of individual fractions (clay, silt, and sand) through the investigated profile. Among the THM, the pyroxene predominates. Mediterr. Crystals of the minerals amphibole, biotite, and feldspar are sometimes visible without magnification. Geoloka I Geomorfoloka Opaanja U Jami Muda Labudova [Geological and Geomorphological Observations in the Muda Labudova Pitin Croatian]. In the wider Mediterranean area, the mineral composition of Terra Rossa type soils and palaeosols may be very variable (Durn, 2003). Numerical dating is also absent. doi:10.1007/s42990-020-00030-9, Sasowsky, I. D., ebela, S., and Harbert, W. (2003). With a summit at 1,109 metres, Mt Pendeli is a great place to climb up to relish a striking view of the Attica basin below, for a start. Thegoal of Ancient Origins is to highlight recent archaeological discoveries, peer-reviewed academic research and evidence, as well as offering alternative viewpoints and explanations of science, archaeology, mythology, religion and history around the globe. doi:10.1111/j.1475-4754.1999.tb00987.x, Garca, J.-L., Maldonado, A., de Porras, M. E., Nuevo Delaunay, A., Reyes, O., Ebensperger, C. A., et al. J. Speleology. Single-grain Dating of Young Sediments Using the pIRIR Signal from Feldspar. Salt Lake City, Utah 84116, Mailing Address: 247, 1024. Within Dinaric karst there are dated cave bear specific sites (e.g., Krina jama) with ages of cave bear thanatocenoses around 4745 ka and >94 ka BP (Bosk et al., 2012). 35 p., B.Sc. 51 Want to Visit? On Fridays and Saturdays from 19:30, the observatory hosts a presentation about outer space and the universe. If the flowstone is allochthonous (e.g., spallation from the ceiling), the obtained age could still be used as the oldest possible date when deposition of the upper section of the DC-SP profile commenced. We recommend booking Davelis Cave tours ahead of time to secure your spot. Artifacts have been found in the cave depicting the god, niches have been cut into the walls and there is an alcove with a pool of water for some unknown purpose. However, due to the thin and discontinuous horizon (Figure 3A), an allochthonous origin is not excluded. Source: Haridimous / Public Domain, Ferro, Shaunacy. Cave deposits and sedimentary processes in Cova des Pas de Vallgornera (Mallorca, Western Mediterranean). The results of the XRPD method are shown in Table 2. The surrounding area was used as a marble quarry by the builders of the Acropolis, and the cave was discovered by chance, during works for the extraction of marble. Bulk and clay mineral Composition Indicate Origin of Terra Rossa Soils in Western Herzegovina. Mica (muscovite) appears only sporadically (<1%) in the form of transparent plates with a rounded outline (Figure 5C). It serves as a habitat for a wide range of river and swamp creatures. Glacial and Periglacial Environments, in The Physical Geography of the Mediterranean. The Mausoleum of Halicarnassus: What Made the First Mausoleum a Wonder? 38, 10931106. The sediment comes from . (2016). Last Glacial Settlement of Croatia: Catalogue of Fossil Sites Dated to the OIS 2&3. This Minecrafty beauty is named Fingal's Cave, Scotland. (1999). Ljetopis JAZU. doi:10.1016/j.earscirev.2005.08.003. Methods Phys. Geologia Croatica. - . Cave bear Killers and Scavengers from the Last Ice Age of central Europe: Feeding Specializations in Response to the Absence of mammoth Steppe Fauna from Mountainous Regions. Clim. PO BOX 146100 (2021). All subsequent analyses could therefore only be conducted for the latter sample. Slate can be seen west of Patters spring in the Pilot Range, Box Elder County. However, the distribution of palynofacies shown on Figure 10 in the lower part of the section, could also be a reflection of palynomorph transport by hydrological mechanism of cave drip water into the vadose cave channel. TABLE 3. Quat. Utah is peppered with volcanoes and other signs of the hot molten rock (magma) that forms within the crust beneath us. (1958). Maximum uplift of the local mountains was calculated of up to 1,200m, with vertical shifts on individual faults averaging from 300 to 500m (Prelogovi, 1975). Equivalent dose values and resulting ages as well as all luminescence results are summarized in Table 3. doi:10.15291/geoadria.23, Marom, A., McCullagh, J. S. O., Higham, T. F. G., and Hedges, R. E. M. (2013). What is also strange about the work done by the mysterious organization is that, after a while, they stopped reinforcing restricted access to the cave and holes were cut through barbed wire. In contrast to potassium-rich feldspar, it is known that only a small fraction of quartz grains (usually <10%, but frequently also down to only few percent) does emit a luminescence signal suitable for dating (e.g., Lthgens et al., 2011). 16, 161170. Samples DC-SP 2, 3 and 5 are classified as very poorly sorted clayey silt, while samples DC-SP 6 and 7 are classified as poorly sorted silt. doi:10.1016/0277-3791(92)90074-I, Georgiadis, I., Chatzopoulou, K., Kantiranis, N., Ioakeimidis, I., and Tsirambides, A. The recent discovery of a 5,000-year-old chalk drum in the UK has transformed our understanding of prehistoric Britain. 65 (1), 2631. If the sediment is buried deeply, it becomes compacted and cemented, forming sedimentary rock. Cro 67 (3), 171183. Davelis Cave. Apart from the panoramic view, the cave itself is a very special sight to explore, if you are an adventurous ad fearless person! FIGURE 5. 546, 419. Non-Pollen Palynomorphs,. During sample preparation, the ends of the cores were removed, because of potential light exposure during sampling. Glad You Asked: What are fulgurites and where can they be found. To aid in their study of the earth, geologists group rocks into three categories based on their origin: igneous, sedimentary, and metamorphic. Many of the picturesque views of the desert southwest show mesas and arches made of layered sedimentary rock. Who would you pick for the best military leaders of all time? Ivanovi, A., Saka, K., Markovi, S., Soka, B., unjar, M., Nikler, L., et al. As weather conditions erode existing rocks, grains of sediment collect and are carried to a sediment deposit, often by means of water or glacial transport. Although the detritus was transported underground by turbulent flows rich in suspended sediment, the final depositional mechanism of this sediment type is very likely related to deposition from stagnant water suspension, as evidenced by the particle size characteristics and the lamination of the sediment. During the Byzantine period, monasteries and churches were built on Mount Penteli. Clastic sedimentary rocks may have particles ranging in size from microscopic clay to huge boulders. Ijs. (2003). It motivates me to keep going on! Common rock types within the intrusive category are granite and diorite. It is true though that the cave, because of its reputation, still attracts occult worshipers during the night. 56 (1), 83100. Weaver, C. E. (1967). J. Sediment - National Geographic Society doi:10.5194/smsps-1-223-2002, Therre, S., Fohlmeister, J., Fleitmann, D., Matter, A., Burns, S. J., Arps, J., et al. Besides fragmentation, the most common taphonomic modification is very light weathering (fine line fractures and spalling of bone surface), while chemical etching is evidenced on several fragments. Common Sedimentary Rocks: Common sedimentary rocks include sandstone . Limestone:Limestone is composed of more than 50% calcium carbonate (calcite). Rev. If you havent yet visited Davelis Cave, now is the time to do so. Also, the relationship between the habitation of bats and HA formation in caves has been found in limestone caves worldwide (Hill and Forti, 1997). doi:10.1002/jqs.2550, Sarkaya, M., Stepinik, U., ebre, M., iner, A., Yldrm, C., Vlahovi, I., et al. Na Razmeu Svjetova Za Prijelaza Milenija: Kasno Bronano Doba Na Kvarneru [At the Crossroads of Worlds at the Turn of the Millennia: The Late Bronze Age in the Kvarnerin Croatian]. (2020). Geomorfoloka Obiljeja Sjevernog Velebita [The Geomorphological Features of Northern Velebit]. Metamorphic rocks are any rock type that has been altered by heat, pressure, and/or the chemical action of fluids and gases. The route to Halandri will take you through the creeks greenery as well as the urban landscape. Additional samples for radionuclide determination were taken in the direct surroundings of the luminescence samples. Some quartzite formations retain their original bedded (layered) structure such that when broken they form flagstones that are commonly used in landscaping or as veneer for buildings. The floor in the almost entire length of the channel is built of sediment and in the upper part it is mostly covered by archaeological layer. Geologists Assoc. Deposition of the Di facies sediments took place during a period of a colder and drier climate (Chapter 4.4). The story of Penteli Cave got even stranger when, in 1977, a group of workers and technicians claiming to be from an unknown organization put up barbed wire around the cave and began to do work on the cave with dynamite and bulldozers. Paleontoloka Istraivanja I Speleoloka Rekognosciranja U 1959 Godini [Paleontological Research and Speleological Reconnaissance in 1959 - in Croatian]. Trek its routes, visit historic monasteries and small waterfalls and then sit at one of the well-known tavernas at its base to enjoy charcoal-grilled chops. doi:10.1016/j.quageo.2012.04.016, Reimer, P. J., Austin, W. E. N., Bard, E., Bayliss, A., Blackwell, P. G., Bronk Ramsey, C., et al. doi:10.1111/j.1502-3885.2011.00211.x, Lthgens, C., Neuhuber, S., Grupe, S., Payer, T., Peresson, M., and Fiebig, M. (2017). Tectonics. The obtained date does not necessarily indicate the time of deposition at the investigated site but the time when the sediment entered the cave environment.
125 Westridge Industrial Blvd Ste 303 Mcdonough, Ga 30253, Articles I