Katon Moyong · Arunachal Press Club, Itanagar · 5 Nov 2026 · Video: The Arunachal Times
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Transcript and contextArunachal Press Club, Itanagar5 November 2026
“No more talks” Katon Moyong on the Siang dam
Days after Delhi Police detained him outside Arunachal Bhawan, the anti-dam activist known as Aborman rejected the government’s invitation to talks on the Siang Upper Multipurpose Project. Scroll to see what is at stake upstream and downstream, then hear him in full.
- 03
Two cases
Government Store water against floods, dry-season shortages and sudden releases from China’s 60,000 MW Medog project upstream.3911
Community Submergence of Adi villages and farmland. Communities also reject the armed deployment used to force survey drilling, and dispute the village MoUs presented as consent.6812
- 04
How it came to this
- The Centre declares a Siang storage project a national project.3
- NHPC drafts a pre-feasibility report on three sites: Dite Dime, Ugeng and Parong.6
- Central forces deploy at Beging for survey drilling, and a dharna begins.8
- Six villages sign MoUs for the survey; some residents dispute them.1314
- The CM invites SIFF to talks. On 23 Oct the NHPC office and a police station in Pasighat are set on fire.161718
- Delhi Police detain about 40 protesters, Moyong among them.1920
- Moyong rejects the invitation to talks.
- 05
Floods come down from Tibet
The case for SUMP rests on what comes down the river from Tibet. Three times in 26 years, a lake that formed suddenly there has burst and flooded the country downstream: on the Siang in 2000, and on Nepal’s Bhote Koshi in July 2025 and again in August 2026.364041
None of the three began at a dam.
- 06
26 August 2026: a mountain falls
Ice and rock broke off the north face of Langtang-Lirung, on the Tibetan side. The avalanche became a debris flow and dammed the Lhende Khola. The lake behind it broke through and sent a surge down the Bhote Koshi and the Trishuli.3637
USGS traced the seismic signal to the collapse itself, so this was neither a dam failure nor a glacial-lake burst.
Keep scrolling to follow the surge. The river line is approximate.
- 07
The cost
0dead in Nepal (Red Cross, 27 Oct). NDRRMA counted 1,367 on 9 Sep 0missing as of 9 Sep 0hydropower projects damaged: 256 MW operating and 3,795 MW under constructionThe flash-flood warning system was tuned to monsoon floods, and its upstream stations were swept away before they could raise an alert. Here the hydropower plants were among the casualties.373839
- 08
It has happened on the Siang
In April 2000 a landslide dammed the Yigong river in Tibet. When the dam gave way in June, it released about 2–3 billion m³ of water. The surge reached Pasighat, 462 km downstream, and raised the Siang by 5.5 m.41
Scroll to follow the surge.
- 09
What China is building at the Great Bend
This chapter draws on a 14-post open-source thread by Kyang Thang (@Kyangs_Thang), 1 Nov 2026. He compiled and translated Chinese netizens’ readings of the project plan shown at the July 2025 inauguration. He notes that Indian media have carried little of this detail.42
The 60,000 MW Medog project is not one wall across the river. It is a chain of three holding dams joined by long diversion tunnels. The river falls more than 2,000 m around the Great Bend, and that drop produces most of the power.942
- 10
Mainling: the big reservoir
The uppermost dam sits near Mainling town (29.2037, 94.0787), on a wide plain at about 2,950 m.
- 130–150 m tall
- ≈16 bn m³ of storage, more than SUMP’s 9.2
- Reservoir up to 3,070 m, kept below the Lhasa–Nyingchi railway that runs nearby
- Construction began July 2025 with an inauguration. Time-lapse imagery shows the site works growing fast.
Source: Kyang Thang’s thread, post 4–7. Open-source estimate, unofficial.42
- 11
Pé: where the river is diverted
At Pé (29.5699, 94.8982), the true entry to the upper gorge, a lower dam would create the storage and diversion reservoir.
- 10–20 m above ground, at 2,900 m
- High water at 2,920 m
- ≈550 million m³
Plans show a new Pé township and a new bridge across the reservoir. The existing bridge could go under.
Source: Kyang Thang’s thread, post 8–9. Open-source estimate, unofficial.42
- 12
Through the mountain, not around it
Between Pé and the lower gorge near Medog, the river loops around Namcha Barwa for well over 150 km. The tunnels would cut across in about 46 km, dropping more than 5,500 ft. Two intermediate cascade stations and holding reservoirs are expected along the way. The route runs parallel to the G219 highway and its Doshong La tunnel.
Orange: the river’s route around the bend. Black: the tunnel, with its two stations. Positions are approximate.
Source: Kyang Thang’s thread, post 10. Open-source estimate, unofficial.42
- 13
Xirang, and a gorge that slides
The last dam, at Xirang (29.2551, 95.1902) near Beibeng township (Drepung in Tibetan), is thought to be a final storage dam that would steady the water coming out of the tunnels. Some groundwork is visible, but its design is not known.42
The gorge is itself unstable. He points to a massive landslide area in the Tsangpo gorge that “sometimes threatens to collapse/flood”, and links to SANDRP’s report on a landslide there on 22 March 2021.42
Source: Kyang Thang’s thread, post 11, 13. Open-source estimate, unofficial.42
- 14
So does Medog store water?
Moyong says China is “not storing the water. They’re just diverting” (17:36). His account of the tunnels matches the thread. But if the netizens’ figures hold, Mainling alone would store about 16 bn m³ and Pé a further 0.55 bn m³.42
On the “water bomb” fear, Kyang Thang writes that he is “not sure if it’s convincing enough”. If the concern is real, he suggests, the government can inform the community, sign a liability waiver and put early-warning systems in place.42
- 15
SUMP: a cushion, if it is kept empty
Yigong surge, 2000: 2–3 bn m³SUMP live storage: ≈9.2 bn m³Mainling, China: ≈16 bn m³ (reported)SUMP could absorb a Yigong-sized surge only if it were held partly empty, while a hydropower reservoir is normally kept full.22541 Nepal shows the other side: a dam in an unstable gorge is itself exposed to the same hazard.
- 16
The Adi heartland
The stretch from Tuting through Yingkiong to Geku is the core of Adi cultural life. Kyang Thang estimates that a 300 m SUMP could submerge more than two-thirds of it, and calls such a dam “quite infeasible: the cons outweighing pros”. Mongabay reports the height at Parong as 250 m; the design is unpublished.426
He also argues the government must explain what hydropower could offer, such as jobs and industry, and discuss alternative sites or smaller cascade dams with the community.42
- 17
Who lives here
The 2011 census counted 1,57,657 Adi, nearly all along the Siang and its neighbouring valleys. Circle area is proportional to each district’s count.21
- 18
And downstream
Below Pasighat the Siang meets the Dibang and Lohit to form the Brahmaputra. In 2011, 2.76 crore people lived in Assam’s Brahmaputra valley, about 175 for every Adi. The river then continues into Bangladesh.22
That ratio is the political arithmetic of the dam, but it measures who is exposed to floods, not who a dam would protect.
- 19
Now hear him
Moyong says the time for talks is over. Below: his argument point by point, the numbers on both sides, what Indian law actually guarantees, and the full 41-minute press conference with a searchable transcript.