Belated comments on Sir Roland Braddell’s Studies of ancient times in the Malay Peninsula
Paul Wheatley’s 1955 article is a critical response to Sir Roland Braddell’s two-decade programme of papers on the ancient geography of the Malay Peninsula, published in the JMBRAS between 1935 and 1951. Writing from the vantage point of post-war Ptolemaic scholarship and emerging geomorphological research, Wheatley argues that Braddell’s identifications of Ptolemaic rivers and place-names rest on outdated textual assumptions and are contradicted by physical evidence, and he proposes alternative solutions to several of the period’s most persistent geographical puzzles.
Summary
Wheatley’s first and most fundamental challenge concerns the nature of the Ptolemaic Geographike Huphegesis itself. Braddell, even in papers written after 1946, relied on Berthelot (1930), Gerini (1909), Rylands (1893), and Bunbury (1879)—all products of a pre-modern era of Ptolemaic studies that treated the text as substantially the work of the second-century Alexandrian. Wheatley surveys the intervening scholarship, culminating in Leo Bagrow’s demonstration that Ptolemy was responsible only for Book I (cartographic theory) and a small appendix in Book VIII, while the 8,000+ coordinates of the habitatilis were compiled by an anonymous Byzantine scholar of the tenth or eleventh century. This re-dating has profound consequences: the Geography can no longer be claimed as the earliest extant account of the Malay Peninsula (Chinese sources in the Liang Shu are older), Indian place-names in its lists cannot be used to date second-century Indian cultural contacts with the Peninsula, and the absence of archaeological evidence from the second century becomes intelligible rather than puzzling.
The second major argument concerns the Ptolemaic river system of the Golden Chersonese, which depicts three streams—Khrysoanas, Palandas, and Attabas—dividing from a common source in the “nameless mountains” of the Peninsula. Braddell had identified these with the Bernam, Pahang, and Johore rivers, invoking the hypothesis that these rivers once flowed from a common source. Wheatley demolishes this on geomorphological grounds, citing Richardson’s work showing that the Malayan drainage pattern was substantially the same in the fifth century A.D. as it is today, and that the only significant Tertiary-period diversion (the Pahang flowing south via the Bera valley) belongs to geological time, not historical time. Instead, Wheatley argues that the Ptolemaic system depicts the well-known Panarikan portage route between the Upper Muar and the Sungei Serting (a Pahang tributary), a route so familiar to sixteenth-century cartographers that no fewer than thirty-two European maps of the period depicted it as a trans-peninsular canal. The Khrysoanas is thus the Muar, the Attabas the Lower Pahang, and the Palandas the Upper Pahang and Jelai rivers, the latter providing access to the Ulu Pahang goldfields.
The final section addresses the Chinese place-name T’ou-chü-li, which Braddell and most scholars had located on the west coast of the Peninsula as the port of departure for a journey to the Ganges. Wheatley draws attention to Fujita Toyohachi’s reinterpretation of the Liang Shu passage, in which the character 投 is read not as part of a toponym but as a verb meaning “to go towards.” This eliminates the hypothetical T’ou-chü-li entirely, permits the identification of Chu-li with Ptolemy’s Kole on the east coast, and resolves the long-standing difficulty of explaining why a journey from the north-west coast to the Ganges should take more than a year—junks rounding the southern tip of the Peninsula routinely waited for the half-yearly monsoon change.
Key Findings
- The Geographike Huphegesis survives in more than forty manuscripts; the earliest extant dates from the twelfth century, and the text was probably compiled in its present form by a Byzantine scholar of the tenth or eleventh century (Bagrow, 1930, 1938, 1945) (pp. 79–83).
- No fewer than thirty-two European maps from the sixteenth and early seventeenth centuries depicted the Muar–Pahang route as a trans-peninsular canal; Godinho de Eredia’s map of 1613 correctly shows the Panarikan portage instead (pp. 90–93).
- Geomorphological evidence (Richardson, 1947, 1949) demonstrates that the Malayan drainage pattern was substantially the same in the fifth century A.D. as today; the Bernam, Johore, and Pahang rivers have not flowed from a common source during the last two thousand years (pp. 89–90).
- The pass from Ulu Slim to the Lipis River basin stands approximately 3,000 feet above sea level, contradicting Dato’ Douglas’s claim of an “easy path” and undermining one of the three factors that led Braddell to choose the Bernam over the Muar (p. 87).
- The Tanjore Inscription (A.D. 1030–1) mentions Talaitakkolam, an identification with Ptolemy’s Takola first proposed by Kanakasabhai in 1902 and now strengthened by the re-dating of the Geography to the same general period (p. 83).
- Fujita Toyohachi’s reading of 投 as a verb in the Liang Shu Wu dynasty passage (222–280 A.D.) eliminates the hypothetical port T’ou-chü-li and permits Chu-li to be identified with Ptolemy’s Kole on the east coast (pp. 96–98).
Conclusion
Wheatley’s definitive takeaway is that the ancient geography of the Malay Peninsula must be reconstructed on the basis of modern textual criticism and physical geography rather than the inherited assumptions of nineteenth-century Ptolemaic scholarship. The Ptolemaic river system is best understood as a schematic representation of the Panarikan trade route, the Geography itself is a Byzantine compilation of uncertain internal dating, and the Chinese sources—properly read—point to the east coast rather than the west as the location of the key port Chu-li.
Context
- The article draws on the Ptolemaic manuscript tradition as classified by Cuntz (1923) and Schnabel (1930, 1938), geomorphological memoirs of the Geological Survey Department (Richardson, 1947, 1949), and a corpus of sixteenth- and seventeenth-century European maps held in the British Museum.
- Historiographically, the piece marks a turning point in Malayan ancient geography by introducing continental Ptolemaic scholarship and physical geography into a debate that had been conducted almost entirely within the framework of Braddell’s earlier JMBRAS papers.