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On impinging on the lithosphere at spreading ridges or in intra-plate settings, mantle plumes may generate hotspots, large igneous provinces and hence considerable dynamic topography. However, the active role of mantle plumes on subducting slabs remains poorly understood. Here we show that the stagnation at 660\u2009km and fastest trench retreat of the Tonga slab in Southwestern Pacific are consistent with an interaction with the Samoan plume and the Hikurangi plateau. Our findings are based on comparisons between 3D anisotropic tomography images and 3D petrological-thermo-mechanical models, which self-consistently explain several unique features of the Fiji\u2013Tonga region. We identify four possible slip systems of bridgmanite in the lower mantle that reconcile the observed seismic anisotropy beneath the Tonga slab (<jats:italic>V<\/jats:italic><jats:sub>SH<\/jats:sub>&gt;<jats:italic>V<\/jats:italic><jats:sub>SV<\/jats:sub>) with thermo-mechanical calculations.<\/jats:p>","DOI":"10.1038\/ncomms10799","type":"journal-article","created":{"date-parts":[[2016,2,29]],"date-time":"2016-02-29T10:04:58Z","timestamp":1456740298000},"update-policy":"https:\/\/doi.org\/10.1007\/springer_crossmark_policy","source":"Crossref","is-referenced-by-count":69,"title":["Upper- and mid-mantle interaction between the Samoan plume and the Tonga\u2013Kermadec slabs"],"prefix":"10.1038","volume":"7","author":[{"given":"Sung-Joon","family":"Chang","sequence":"first","affiliation":[]},{"given":"Ana M. 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