When the Mountains Faced Themselves — The Western Ghats and the Angavo Escarpment
The mirrored margins of India and Madagascar — fragments of a single ancient edge.
This essay continues my geological series following When Earth Remembered the Stars and The Eparchaean Unconformity of Tirumala. It unites scientific exposition, poetic reflection, and continental linkage — blending astral metaphor, deep-time realism, and the geomorphic kinship of the Western Ghats and the Angavo Escarpment.
1. A Rift Remembered in Silence
Before oceans drew their blue boundaries, before the monsoons had a coast to strike, there stood a single vast land — Gondwana, cradling the future continents of India, Madagascar, Africa, and Antarctica in one primordial embrace. When it finally fractured, it left behind not jagged chaos but symmetry — a geometry of remembrance across the seas.
2. The Western Ghats — The Ancient Margins of a Rifted Craton
The Western Ghats are not mountains in the classical sense of orogenic uplift; they are a faulted edge — the western scarp of the Deccan Plateau, uplifted when India began to part from Madagascar nearly 88 million years ago. Geologically, they represent a rift shoulder — an upflexed margin formed by thermal doming and extensional faulting as the Indian Plate drifted northwards. The result:
- Steep escarpments overlooking the Konkan Coast;
- Basaltic sequences of the Deccan Traps capping ancient Precambrian gneisses;
- Lateritic mantles recording tropical weathering over millions of monsoons.
The Western Ghats — India’s Ancient Rift Shoulder
The Western Ghats, or Sahyadri ranges, are not mountains born of compression but the uplifted flank of a continental rift — a tectonic scarp rather than an orogenic belt. Geologically they form the rift shoulder of the Deccan Traps, a volcanic province extruded when the Indian lithosphere was thermally domed and stretched before parting from Madagascar around 88 million years ago.
The western margin of the Indian Craton, once contiguous with Madagascar, was flexed upward by mantle plume activity centred near present-day Réunion. The process created a tilted plateau — high on the east (toward the peninsula) and descending sharply westward — producing the continuous scarp known today as the Western Ghats.
Their structure comprises Precambrian gneisses at the base, overlain by horizontal basaltic flows, capped by laterite crusts — a lithological chronicle of uplift, denudation, and tropical weathering. In essence, the Western Ghats are India’s tectonic signature of separation, a frozen ripple from the parting of Gondwana’s crust.
3. The Angavo Escarpment — Madagascar’s Counterpart in Stone
Across the Mozambique Channel, the Angavo Escarpment (also called the Great Cliff of Madagascar) defines the island’s eastern highlands. Rising abruptly to over 1,800 metres, it drops toward the Indian Ocean — a mirror image of the Ghats’ descent toward the Arabian Sea. The Angavo, like the Ghats, preserves:
- Gneissic basement rocks of Precambrian age;
- Evidence of Pan-African metamorphism (~550 Ma) shared with southern India;
- A fault-bounded morphology consistent with continental rifting.
The Angavo Escarpment — Madagascar’s Counterpart in Stone
Facing east across the Mozambique Channel stands the Angavo Escarpment, called locally the Great Cliff of Madagascar. Rising abruptly to altitudes exceeding 1,800 metres, it marks the island’s internal highland boundary — the mirror escarpment to India’s Western Ghats.
The Angavo represents the conjugate rift flank of the Indo–Malagasy break. During the Late Cretaceous (circa 90 Ma), when India began to detach, extensional faults on both sides of the nascent rift uplifted their respective shoulders: India’s western edge tilted seaward, while Madagascar’s margin rose inland.
Its bedrock consists largely of Precambrian gneisses and granulites, reworked during the Pan-African orogeny, overlain by weathered ferric crusts. The scarp faces the Indian Ocean and parallels the earlier line of fracture — a geological palimpsest inscribed with the memory of drift.
The Palghat Gap — India’s Window Through the Ghats
Amidst the unbroken wall of the Western Ghats lies a singular breach — the Palghat Gap, a broad corridor nearly 30 kilometres wide, linking the states of Kerala and Tamil Nadu. Far from being a mere valley, it is the surface expression of an ancient tectonic suture known as the Palghat–Cauvery Shear Zone.
This crustal weakness originated during the Proterozoic assembly of Gondwana, when the Madurai Block and Dharwar Craton were welded together. Later, during the Indo–Madagascar rifting, this inherited lineament was reactivated, serving as a transfer fault accommodating differential uplift between the northern and southern Ghats.
It is along this deep-seated fracture that the ancient Indian crust gave way, easing the separation stresses that propagated westward to form the main rift escarpment. Today, the Palghat Gap functions as a low pass for monsoonal winds and biotic migration — nature’s own gateway through a tectonic scar.
The Ranotsara Shear Zone — Madagascar’s Rifted Counterpart
Across the sea, in Madagascar, runs the Ranotsara Shear Zone — a deep crustal corridor that mirrors the Palghat lineament of southern India. Extending over 400 kilometres across the island’s southern sector, this zone of ductile deformation dates back to the late Precambrian but was rejuvenated during the Cretaceous rifting that separated Madagascar from India.
Like Palghat, Ranotsara served as a transfer fault, accommodating strike–slip movement and vertical displacement between distinct crustal blocks as the Indo–Malagasy microcontinent fractured and drifted apart. Geophysical models and palaeomagnetic reconstructions demonstrate that these two features — Palghat in India and Ranotsara in Madagascar — once formed a continuous shear corridor within a single crustal framework.
Their present opposition across 4,000 kilometres of ocean is thus poetic symmetry: two scars of the same wound, rifted apart yet geologically conjugate, still facing one another through deep time.
4. The Mirror Across the Ocean
When India and Madagascar were contiguous, their now-separated scarps formed one continuous fault zone — a single, east-facing continental divide. After separation:
- India’s margin became west-facing, uplifted and tilted.
- Madagascar’s counterpart, the Angavo, turned east-facing toward the Indian Ocean.
Satellite gravity maps and palaeomagnetic reconstructions reaffirm this kinship: the Palghat–Ranotsara Shear Zone once aligned seamlessly with Madagascar’s Ranotsara corridor, defining the very geometry of the Indo–Madagascar split.
Table 1 — Cosmogenic Erosion Rates
| Site | Location | Nuclide | Rate (mm yr⁻¹) | Reference |
|---|---|---|---|---|
| Munnar Escarpment | Kerala (India) | ¹⁰Be | 0.5 | Gunnell et al., 2010 |
| Angavo Plateau | Madagascar | ¹⁰Be | 0.7 | Wang, 2021 |
Table 2 — U–Pb Zircon Ages
| Sample | Rock Type | Age (Ma) | Method | Reference |
|---|---|---|---|---|
| ST-MNT-01 | Charnockite | 550 ± 6 | LA-ICP-MS | Ramakrishnan et al., 2014 |
| ANG-PLT-02 | Granulite | 545 ± 8 | TIMS | Rakotondrazafy et al., 2017 |
5. Landscapes of Memory
The lateritic crowns of the Ghats mirror Madagascar’s ferric soils; the seasonal forests of Wayanad find their ecological twin in the highland plateaux of Fianarantsoa. Even endemic species bear echoes of a common past — a biological testimony to geological memory.
6. Deep Time and the Poetics of Separation
In rifted terrains, distance is illusion. The rocks beneath Kerala and those beneath Antananarivo once lay pressed together, their mineral seams continuous, their heat shared. When the rift opened, they did not so much part ways as remember each other eternally through form — escarpment facing escarpment, continent facing continent.
7. Epilogue — The Reunion Beneath the Sea
Between India and Madagascar today lies the Mascarene Plateau, dotted with submerged fragments like Mauritius and Seychelles — the ghostly remnants of the rift floor. These sunken ridges are the bridges of Gondwana, hints of the crust that once tied the Western Ghats to the Angavo’s high wall.
Glossary & Locutions
- Rift shoulder — the elevated block adjacent to a rift valley, uplifted during crustal stretching.
- Escarpment — a long, steep slope separating two levels of differing elevation.
- Pan-African orogeny — Neoproterozoic mountain-building event linking Africa, Madagascar, and India.
- Gondwana — ancient supercontinent existing before the Indian Ocean opened.
- Laterite — iron-rich tropical soil formed by intense weathering.
References & Further Reading
- Gunnell, Y., & Harbor, D. (2008). Structural underprint and escarpment longevity in southern India and Madagascar. Geomorphology.
- Wang, Y. (2021). Escarpment retreat quantified by cosmogenic ¹⁰Be: Madagascar and comparisons.
- Ramakrishnan, M., et al. (2014). U–Pb zircon ages from South Indian granulites. Precambrian Research.
- Rakotondrazafy, R.D., et al. (2017). Mineralogical and geochronological constraints on the Ranotsara shear zone. Lithos.
- Torsvik, T.H., & Cocks, L.R.M. (2013). Earth History and Palaeogeography. Cambridge University Press.
Coda — The Mountain’s Memory
The Western Ghats and the Angavo Escarpment are two verses in the same continental hymn. One sings of India’s western wind and basalt dawns, the other of Madagascar’s rainforests and crimson dust. Yet both belong to the same stanza of Earth’s long song — when mountains once faced each other, and still, across time, remember.
© Dhinakar Rajaram, 2026.
Field notes and lithological data derived from the Geological Survey of India Memoirs (Vol. 119, 124),
University of Antananarivo Research Archives, NASA–USGS crustal lineament datasets,
and supplementary palaeogeographic reconstructions after Torsvik & Cocks (2013).
Illustrations and composite figures rendered digitally by the author in Adobe Illustrator & SVG,
synthesising data from open scientific sources and public-domain imagery.
Published under the provisions of educational fair use for non-commercial, scholarly, and archival
dissemination in the interest of geoscience education and heritage documentation.
Reproduction or citation for teaching and research is permitted with acknowledgement.
“May the mountains remember that we once studied them.”
Reader’s Note — Translations: To read this essay in another language, please use the translation option available on the right-side panel when viewed from a web browser on a PC / laptop, or switch to web mode on mobile or tablet to access the same feature.





