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**Scientific analysis based on the primary source:** Mildner, S. (2025/2026). *A new interpretation of Ptolemy's Germania Magna: Employing computer-assisted image distortion of a medieval map by Donnus Nicolaus Germanus to examine post-glacial geodynamics in Europe*. EarthArXiv (Preprint). https://doi.org/10.31223/X5313T
([📥 **Download v5.0-PDF**](https://eartharxiv.org/repository/view/8484/))

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Last updated: to Version v6 (May 24, 2026)
([📥 **Download NEW v7.3-PDF**](https://zenodo.org/records/20474381/files/Geodynamic_Model_Description_for_Ptolemys_Germania_Magna___eartharxiv__7.3.pdf?download=1))

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The historical geography of Germania Magna remains one of the most challenging fields in classical studies and geodetic research. The currently paradigmatically influential reference model — the statistical-geodetic rectification of the TU Berlin group (Karlsen et al., 2011) — explains deviations between Ptolemaic coordinates and modern topography primarily as measurement errors of ancient instruments or as transmission artefacts.

The present model is based on a fundamentally opposing assumption. The primary explanatory principle is the recognition that the northern reference coastline of the Oceanus Germanicus lay approximately 120 km further south in antiquity. Medieval cartographers projected Ptolemy’s coordinates onto a landscape already altered by major 6th-century geodynamic processes. This produced a systematic northward stretching of the map image and a corresponding eastward displacement of eastern coordinates.

The cartometric foundation — a strictly affine transformation anchored on the invariant Rhine–Elbe baseline with a global scaling factor of ≈28 km per Ptolemaic degree of longitude — remains unchanged. The statistically irrefutable −93.1 km eastward displacement of the Elster Cluster is the empirical core result.

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**Scientific supplementary analysis to:** Mildner, S. (2025/2026). *A new interpretation of Ptolemy's Germania Magna*. EarthArXiv (Preprint). https://doi.org/10.31223/X5313T
([📥 **Download v5.0-PDF**](https://eartharxiv.org/repository/view/8484/))

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Note: The geophysical evidence analysis below remains valid for v6. Section 4.2 uses an 8-point subset; the v6 main paper (tab. cesky_zones) expands this to n = 14 with p ≈ 3.4 × 10⁻⁵. The kinematic terminology (Section 8) reflects v5; v6 additions (K4 anchor, G7 biaxial extrusion) are documented in the main v6 paper only.

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***Disclaimer***

*This article presents an interdisciplinary working hypothesis that integrates cartometry, geodynamics, sedimentology, and historical sources. It proposes a geodynamic and climatic rupture in the 6th century AD and formulates concrete, falsifiable predictions. The model challenges aspects of the current mainstream interpretation and is intended to stimulate further empirical testing. It does not claim to be a definitive reconstruction.*

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## 1. Synthesis of Evidence Chains: The Necessity of an Integrated View

The statistically secured findings of the preceding residual analysis – a highly significant eastward offset of the Elster-Lusatia Cluster of $\overline{\Delta}_\lambda \approx -93{.}1$ km ($t = -13{.}7$, $p < 0{.}001$) and the geochemical convergence of the cartometric identification *Budorigum* = Doberlug-Kirchhain with the local anthracite stress metamorphism anomaly – demand a geophysical explanation that goes beyond a purely statistical coordinate analysis. The four key publications under consideration (Nielsen et al., 2007; Arfai et al., 2018; Götze et al., 2023/2024; Weninger et al., 2008), together with Kužvart (1992) and Geersen et al. (2024), provide methodologically heterogeneous but independently derived building blocks that are systematically evaluated below and synthesised with the Mildner model. Particular attention is devoted to the Mercator map cited by Mildner, which shows a landmass named *Albionis Pars* in the *Oceanus Germanicus*, and to the hypothesis that a triggered tsunami may have contributed to an additional northward migration of the coastline through sediment deposition along the North German coast.

The scholarly engagement with Claudius Ptolemy’s Geographike Hyphegesis, particularly regarding the territory of Germania Magna, has faced a fundamental paradox for centuries. While the mathematical coordinates in Ptolemy’s atlas suggest an apparently precise mapping, the described landmarks, river courses, and settlement points can often only be reconciled with the present-day topography of Central Europe through considerable distortion. Traditional research has usually resolved this problem by assuming measurement errors on the part of the ancient sources or by allowing generous interpretive latitude in the identification of hydronyms and toponyms. The researcher Sven Mildner, however, takes a radically different approach in his work: he postulates that the Ptolemaic data are not primarily erroneous, but that the modern interpretation rests on a fundamental misconception about the stability of the European landscape and an incorrect cartographic projection.¹

At the heart of Mildner’s thesis is the re-identification of the Vistula Fluvius. While established historiography invariably equates the Vistula with the present-day Vistula (Weichsel) in Poland, Mildner’s computer-assisted distortion analyses of medieval maps indicate that the ancient Vistula actually describes a river system in what is now eastern Germany, encompassing the Black Elster, the Spree, and parts of the Oder.¹ This westward shift of the central eastern boundary river of Germania Magna by several hundred kilometers has far-reaching consequences for the entire historical geography of Central Europe. It necessitates a re-evaluation of the settlement areas of Germanic tribes such as the Lugii, Burgundians, and Vandals, as well as an explanation of how such a prominent hydronym could “migrate” eastward in the transmitted record.²

The methodological foundation of this re-evaluation is the realization that geodynamic processes, climatic caesuras, and cartographic transmission errors interacted synergistically. The image of Germania Magna was fragmented in the 6th century AD by an unprecedented ecological and demographic catastrophe. The resulting settlement hiatus led to a break in the oral tradition of landscape designations.² When medieval cartographers such as Donnus Nicolaus Germanus began to reconstruct the ancient knowledge, they projected the Ptolemaic coordinates onto a changed physical world and thereby created the distortions that Mildner describes in his new interpretation.²

The study of Claudius Ptolemy’s Geographike Hyphegesis, written around 150 AD, represents one of the most complex tasks in historical geography. With over 6,300 recorded places and their coordinates, the work forms the fundamental framework for our understanding of the ancient world.¹ The scholarly challenge arises from the discrepancy between the ancient data and modern topography, which has historically often been attributed to faulty transmission or insufficient measurement accuracy. The plausibility analysis presented here addresses a radical paradigm shift: the identification of the ancient Vistula not with the Weichsel (Vistula) in Poland, but with the system of the Black Elster in present-day Lusatia, as postulated by Sven Mildner in his publication on Germania Magna.²

This approach is based on the realization that Ptolemy calculated with an Earth circumference of 180,000 stadia, which led to a systematic distortion of the coordinates.¹ Modern research, particularly projects at the Technical University of Berlin by Kleineberg, Marx, and Lelgemann, has shown that more precise localization of ancient settlements is possible through mathematical rectification and statistical analyses.⁴ Sven Mildner’s reinterpretation expands this geodetic framework by incorporating interdisciplinary parameters from geodynamics and archaeometallurgy to create a coherent landscape reconstruction of Germania Magna.³