Understanding the geological processes in Iceland and elsewhere, both tectonic drift and mantle currents have to be considered.
This map shows it all, tectonic drift vectors from the National Land Survey of Iceland. The grid of division lines superimposed on this map shows the outlines of convection rolls below Iceland. The convection rolls can not be measured yet, due to several reasons.
5 Core Factors + 2 Observables:
5 CORE FACTORS (causes in the mantle)
Temperature
Composition (chemistry)
Pressure / depth
Mineral phase (structure)
Partial melt / fluids
2 OBSERVABLES (what we measure)
Seismic velocity (Vp, Vs)
Attenuation (Q)
An addition to low resolution, these factors make it too complicated to get a clear picture of the vertical structure aspects of the mantle. But the methods used here to make the convection rolls model are a shorter way, thereby deducting these lines before modern sensors, relevant AI and other types of technology provide direct observation opportunities.
Each of those lines shows the division between two convection rolls, found below Iceland at different depth, but all of them affect the tectonic plates of N-America and Eurasia. The first demonstration is how the volcanic zones follow the scope of the convection rolls. The only way to explain this consistency is finding out how those division lines affect the tectonic plates (and the crust). Ignoring this consistency would be wrong.
This leads us to consider further what happens down below, within the asthenosphere, the transition zone of the mantle, and the lower mantle. These lines are really narrow and sharp, so the way magma ascends through the tectonic plate should be analysed. The only way is the accumulation of martial melt exactly where the division lines are found, a mechanism of the convection rolls to release the partial melt there and make it possible for the lines of ascending magma to proceed all the way upwards, a distance of 120 km.
With this in mind, a myriad of geological features can be explained, hitherto hidden and not understood.
As can be seen on the map, the tectonic drift vectors are remarkably parallel to the convection rolls. This is a mathematical coincidence, found at the starting point of tectonic drift of the two plates. Farther out, this consistency is not seen, as the two plates drift and rotate in their independent ways.
It can be difficult to explain how peridotite undergoes partial melting to produce basalt, and how that basalt subsequently migrates upward through the lithosphere. Within the asthenosphere, there are no open voids or fractures through which melt can simply flow. Therefore, an important question is how the melt becomes concentrated and how it is transported upward through the ductile portion of the tectonic plate.
Partial melting of peridotite and the subsequent flow of basalt towards the surface
This schematic proposes that partial melting occurs in regions where pressure is reduced due to tectonic movements above. In addition, the interaction of adjacent convection rolls should combine their thermal influence with symmetric heat radiation, creating localized zones where conditions are favorable for partial melting.
The upward transport of melt through the ductile lithosphere must be assisted by some focusing mechanism, allowing it to move in narrow, directed pathways. Evidence for such pathways is found in the sheeted dike complexes within ophiolites, which could represent the uppermost expressions of these ascending melt channels.
One possible physical analogy is the Munroe effect, in which energy is focused into a narrow jet capable of penetrating solid material. In this context, a comparable mechanism might involve the concentration of thermal energy or stress along specific lines or zones, enabling sustained, directed upward flow through the ductile material. The symmetrical flow lines do then have to provide an appropriate “standoff”, a key concept regarding the physical preconditons of Munroe effect. Some might say that explosion on one hand and a steady process on the other hand are not comparable, but considering that the process is the same, even though one is short term, the other long term, the results will be similar.
Beneath oceanic plates, where the lithosphere is approximately 100 km thick, such focused flow could allow basaltic melt to traverse the ductile region. Upon reaching the brittle upper lithosphere, the melt would then exploit fractures and fissures, continuing its ascent.
Finally, as pressure decreases, volatiles exsolve from the magma, causing rapid expansion and increased buoyancy, which further drives the magma toward the surface or the seafloor.
The internal energy flow of the Earth can be approached through a set of simple but physically meaningful preconditions that together form a coherent conceptual model.
The first precondition is that radioactive decay supplies an energy output comparable to the total heat flux emitted by the Earth. This assumption is supported by geochemical evidence suggesting that the abundance of radioactive isotopesโparticularly uranium-238, thorium-232, and potassium-40โin primitive meteorites is broadly consistent with the inferred composition of the Earth. If so, radioactive decay could account for the entirety, of Earthโs present-day heat loss.
The second precondition is that the mantle is partially transparent to thermal radiation, particularly the radiation produced by these radioactive elements, along with the outer core. Under this assumption, a portion of the radiative energy generated within the mantle can propagate downward and be absorbed by the inner core. In this framework, the inner core is not merely a passive reservoir of residual heat, but an active participant in a dynamic energy exchange system.
Energy received by the inner core is then redistributed through convection within the outer core, which acts as an efficient transport mechanism. This convective motion transfers heat upward toward the mantle across the coreโmantle boundary (CMB), a region that plays a critical role in coupling deep Earth processes. From there, heat continues to move through the mantle by a combination of convection and radiation, ultimately reaching the base of the lithosphere.
Within the tectonic plates, heat is transported toward the surface through conduction and localized magma flow, giving rise to volcanic and tectonic activity. In this way, the model provides a continuous pathway for energy: from radioactive sources, through radiative transfer and convection, to surface expression.
A central point of debate concerns the radiative properties of the mantle. Conventional models often assume that the mantle is largely opaque to thermal radiation, which limits the role of radiative heat transfer. However, this assumption remains uncertain, particularly under the extreme temperatures and pressures of the deep mantle. If the mantle is more transparent than typically assumed, radiative energy transfer could play a significantly large role in Earthโs internal energy budget.
Another debated issue is whether the inner core is growing over time. Some models suggest gradual solidification of the core, while alternative perspectives argue that the core maintains relatively stable proportions and temperature through long-term dynamic equilibrium. If such stability holds, it would support a model in which energy inputโpotentially via radiative transferโis balanced by outward heat flow.
To explore the implications of this framework, convection rolls can be introduced into mantle layers as a simplified representation of large-scale flow. These structures provide a useful basis for comparison with observed surface patterns, such as tectonic plate boundaries, volcanic distributions, and heat flow variations. Preliminary comparisons, shown here, suggest that such models may reproduce certain large-scale features of the Earthโs surface, indicating that the approach is worthy of further investigation.
Basic convection rolls model, equatorial section
Conclusion
This holistic model proposes a testable alternative framework for understanding Earthโs internal energy flow. Its validity depends on key assumptionsโsuch as the radiative transparency of the mantle and the long-term stability of the coreโwhich can, in principle, be evaluated through observation, experiment, and modeling. The consistency between the mantle convection roll model and observed surface features has been rigorously tested here and shows strong agreement.
At first glance, eastern Indonesia and the East African Rift appear to have little in common. One is dominated by deep ocean trenches and subduction zones, while the other is defined by continental rifting and volcanic valleys.
Yet when examined more closely, and positioned relative to specific longitudinal reference points, a striking structural similarity emerges.
Similarities and coherence along equator between Great Rift Valley and East Indonesia, with Amazon Estuary included.
Two locations, separated by exactly 90ยฐ in longitude (128.9ยฐE in Indonesia and 38.9ยฐE in East Africa), reveal comparable patterns of tectonic division. In both regions, deformation is not concentrated along a single boundary but instead distributed across multiple, parallel or opposing systems.
This raises an important question: Are these similarities coincidental, or do they reflect deeper, global-scale organization within Earthโs mantle?
The Indonesian Reference Point: A Rare Double Subduction System
The calculated convection rolls grid superimposed on a map showing the Molucca Sea and the related subduction zones.
The point at 128.9ยฐE lies just south of the Philippine Trench, within one of the most tectonically complex regions on Earth.
Immediately to the west lies the Molucca Sea region, characterized by a highly unusual configuration:
Two opposing subduction zones
Oceanic crust being consumed from both sides
Formation of colliding island arcs
This system is often described as a double subduction zone, where the Molucca Sea plate is being subducted both eastward and westward.
Key structural feature:
Deformation is split into multiple opposing boundaries rather than a single subduction interface
The African Reference Point: A Bifurcating Continental Rift
At 38.9ยฐE, we encounter the East African Riftโa region where the African continent is actively splitting apart.
Unlike Indonesia, this is a divergent system, yet it shows a comparable structural division:
The rift splits into two distinct branches:
Eastern Rift
Western Rift
These branches run roughly parallel, enclosing a broad zone of deformation
Key structural feature:
Extension is distributed across multiple rift valleys instead of a single division.
Structural Similarity: Different Processes, Same Geometry
Despite their very different tectonic regimes, both regions share a common structural pattern:
Feature
Eastern Indonesia
East Africa
Tectonic regime
Convergent (subduction)
Divergent (rifting)
Structure
Opposing trenches
Parallel rift branches
Deformation style
Compression
Extension
Common trait
Multi-branch division
Multi-branch division
Insight:
In both cases, the lithosphere does not deform along a single boundary. Instead, it splits into multiple systems.
A Mantle Perspective: Distributed Deformation and Flow Organization
Both regions are located above areas of intense mantle activity:
Eastern Indonesia sits at the intersection of multiple major plates and microplates
East Africa overlies a mantle upwelling.
Within the framework of large-scale mantle convection:
Flow is not necessarily localized
Instead, it may organize into Reylaigh-Bรฉnard type of convection rolls, very well known in physics.
These can produce zones of regular deformation at the surface
Hypothesis
Regions of strong mantle flow may not produce a single tectonic boundary, but instead generate paired or multiple systems, reflecting the motion in the overlying lithosphere.
In this view:
The double subduction in Indonesia (with two others just north and south of there)
And the dual rift system in Africa
โฆare different surface expressions of a similar underlying principle: Deformation partitioning driven by large-scale mantle dynamics
Beyond Coincidence
The comparison between these two regions suggests that:
Complex tectonic features may follow recurring structural patterns
These patterns may not depend on whether the regime is compressional or extensional
Instead, they may reflect how mantle flow organizes lithospheric deformation
This aligns with a broader idea:
Earthโs surface tectonics, as in this case, may be better understood not as isolated plate boundaries, but as parts of a coherent, global system of mantle-driven structure
At approximately 51.1ยฐW, 90ยฐ west of East Africa, lies the Amazon River estuary.
Unlike the other two regions, this is not an active plate boundary. It is part of a passive continental margin. However, it is far from simple.
Key characteristics include:
One of the largest sediment discharge systems on Earth
The Amazon deep-sea fan extending far into the Atlantic
A margin shaped by long-term interaction between:
Continental structure
Ocean basin evolution
Sediment loading and flexure
While not tectonically โactiveโ in the same way, it represents a major function of mass redistribution and lithospheric response, and therefore its location can be connected with local lithospheric preconditions.
A Three-Point Pattern
We now have three locations:
128.9ยฐE โ Eastern Indonesia (double subduction)
The apparent symmetry between eastern Indonesia and the East African Riftโhighlighted by their 90ยฐ longitudinal separation and shared multi-branch structureโinvites a deeper, while the tectonic mechanisms differ, the structural resemblance is difficult to ignore. Adding the Amazon estuary, also with 90ยฐ longitudinal separation as compared with the East African Rift, this arrangement must be regarded as based on something else than coincidence. It should be kept in mind that all those locations are found exactly on the equator.
Rather than viewing these regions as unrelated anomalies, they may represent:
Different manifestations of a common, deep currents within Earthโs mantle
Geodetic measurements show that plate separation across Iceland is directed approximately N15ยฐE (equivalent to ~105ยฐ azimuth). This regional extension is commonly illustrated on geological maps by symmetrical vectors on either side of the island.
Yet the structural grain of the East Volcanic Zone at ~64ยฐN trends N42ยฐE, implying a misalignment of about 27ยฐ relative to the plate motion vector.
In classical fracture mechanics, extension should generate rifts perpendicular to the direction of maximum tensile stress. The observed geometry in Iceland therefore indicates that additional controls modify the stress field within the crust.
One plausible mechanism is the influence of organized **mantle convection patterns. If the upper mantle is structured into long, coherent convection rolls, their boundaries may impose a polygonal framework on the lithosphere. These boundaries can act as zones of mechanical weakness, guiding the localization and ุงุชุฌุงู of rifting.
In this framework, the regional plate-separation vector (N15ยฐE) is not directly expressed at the surface. Instead, extension is effectively reprojected along the geometry of convection-driven domains, producing rift segments such as the East Volcanic Zone with an orientation of N42ยฐE.
A map published by Iceland GeoSurvey, showing inferred convection-roll division lines, highlights this systematic angular discrepancy.
Map showing basic alignment of volcanic and seismic zones, along with the two vectors of plate separation.
