IBOV 177,284 ▼ 0.61% IPSA 10,421 ▼ 0.58% IPC MEX 67,977 ▼ 1.78% MERVAL 2,707,869 ▼ 1.44% COLCAP 2,118 ▼ 0.22% BVL PERÚ 19,767 ▲ 0.37% USD/BRL 5.05 ▼ 0.01% USD/MXN 17.33 ▲ 0.10% USD/CLP 908.88 ▲ 1.38% USD/COP 3,791 — 0.00% USD/PEN 3.43 ▼ 0.01% USD/ARS 1,395 — 0.00% USD/UYU 40.07 — 0.00% USD/PYG 6,066 — 0.00% USD/BOB 6.86 — 0.00% USD/DOP 59.15 — 0.00% USD/CRC 451.24 — 0.00% USD/GTQ 7.62 — 0.00% USD/HNL 26.61 — 0.00% USD/NIO 36.62 — 0.00% USD/VES 516.67 ▼ 0.13% USD/PAB 1.00 ▲ 2.16% USD/BZD 2.00 ▲ 1.59% USD/JMD 157.28 ▲ 0.43% USD/TTD 6.74 ▲ 1.22% EUR/BRL 5.89 ▲ 0.19% BRENT 109.26 ▲ 3.35% WTI 101.02 ▼ 0.15% IRON ORE 161.91 — — COPPER 6.30 ▼ 4.15% GOLD 4,562 ▼ 2.48% SILVER 77.55 ▼ 8.67% SOY 1,177 ▲ 0.21% CORN 455.75 ▲ 0.94% WHEAT 635.75 ▼ 1.74% COFFEE 258.75 ▼ 12.12% SUGAR 14.78 ▼ 1.40% ORANGE JUICE 170.05 ▼ 6.21% COTTON 80.33 ▼ 4.30% COCOA 4,109 ▼ 1.91% BEEF 247.93 ▼ 1.65% CATTLE 361.45 ▼ 1.67% LITHIUM 84.08 ▼ 3.30% PETR4 45.47 ▲ 1.04% VALE3 83.50 ▲ 0.76% ITUB4 39.70 ▼ 1.73% BBDC4 17.69 ▼ 0.84% ABEV3 15.69 ▼ 0.51% BBAS3 20.70 ▼ 0.29% B3SA3 16.70 ▼ 1.36% WEGE3 43.13 ▼ 1.35% PRIO3 68.80 ▲ 2.24% SUZB3 41.70 ▼ 2.16% RENT3 42.98 ▼ 2.18% AZZA3 19.05 ▲ 1.06% CSAN3 4.41 ▼ 5.16% RAIZ4 0.45 ▲ 2.27% PCAR3 2.26 ▼ 1.74% GMAT3 4.34 ▲ 1.17% PSSA3 47.92 ▼ 1.60% CVCB3 1.81 ▼ 4.23% POSI3 3.88 ▼ 2.27% SLCE3 17.19 ▼ 0.87% NATU3 9.94 ▲ 1.53% BRKM5 12.21 ▲ 0.49% RANI3 7.85 ▼ 0.25% CSNA3 6.42 ▼ 3.75% CMIN3 4.72 ▼ 1.05% USIM5 9.12 ▼ 7.79% GGBR4 23.34 ▼ 1.02% ENEV3 25.06 ▼ 3.43% NEOE3 33.80 — 0.00% CPFE3 44.52 ▼ 1.53% CMIG4 11.27 ▼ 0.09% EQTL3 38.59 ▼ 0.54% LREN3 13.55 ▼ 1.24% VIVT3 35.52 ▼ 0.20% RAIL3 14.97 ▼ 1.96% KLABIN 16.43 ▼ 2.55% RAIA DROGASIL 19.59 ▼ 0.25% RDOR3 34.84 ▲ 0.26% HAPV3 12.45 ▼ 6.11% FLRY3 15.60 ▼ 2.26% SMTO3 18.25 ▼ 0.82% UGPA3 29.13 ▼ 1.42% VBBR3 33.12 ▼ 0.81% BBSE3 34.12 ▼ 1.04% BPAC11 54.50 ▼ 1.61% CURY3 30.37 ▼ 0.75% AERI3 2.42 ▼ 0.41% VIVARA 22.94 ▼ 0.26% COMPASS 25.90 ▼ 1.89% VAMOS 3.41 ▼ 2.29% SANB11 26.92 ▼ 0.81% ASAI3 8.50 ▼ 1.05% SBSP3 29.03 ▼ 1.66% WALMEX 54.82 ▲ 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0.01% USD/MXN 17.33 ▲ 0.10% USD/CLP 908.88 ▲ 1.38% USD/COP 3,791 — 0.00% USD/PEN 3.43 ▼ 0.01% USD/ARS 1,395 — 0.00% USD/UYU 40.07 — 0.00% USD/PYG 6,066 — 0.00% USD/BOB 6.86 — 0.00% USD/DOP 59.15 — 0.00% USD/CRC 451.24 — 0.00% USD/GTQ 7.62 — 0.00% USD/HNL 26.61 — 0.00% USD/NIO 36.62 — 0.00% USD/VES 516.67 ▼ 0.13% USD/PAB 1.00 ▲ 2.16% USD/BZD 2.00 ▲ 1.59% USD/JMD 157.28 ▲ 0.43% USD/TTD 6.74 ▲ 1.22% EUR/BRL 5.89 ▲ 0.19% BRENT 109.26 ▲ 3.35% WTI 101.02 ▼ 0.15% IRON ORE 161.91 — — COPPER 6.30 ▼ 4.15% GOLD 4,562 ▼ 2.48% SILVER 77.55 ▼ 8.67% SOY 1,177 ▲ 0.21% CORN 455.75 ▲ 0.94% WHEAT 635.75 ▼ 1.74% COFFEE 258.75 ▼ 12.12% SUGAR 14.78 ▼ 1.40% ORANGE JUICE 170.05 ▼ 6.21% COTTON 80.33 ▼ 4.30% COCOA 4,109 ▼ 1.91% BEEF 247.93 ▼ 1.65% CATTLE 361.45 ▼ 1.67% LITHIUM 84.08 ▼ 3.30% PETR4 45.47 ▲ 1.04% VALE3 83.50 ▲ 0.76% ITUB4 39.70 ▼ 1.73% BBDC4 17.69 ▼ 0.84% ABEV3 15.69 ▼ 0.51% BBAS3 20.70 ▼ 0.29% B3SA3 16.70 ▼ 1.36% WEGE3 43.13 ▼ 1.35% PRIO3 68.80 ▲ 2.24% SUZB3 41.70 ▼ 2.16% RENT3 42.98 ▼ 2.18% AZZA3 19.05 ▲ 1.06% CSAN3 4.41 ▼ 5.16% RAIZ4 0.45 ▲ 2.27% PCAR3 2.26 ▼ 1.74% GMAT3 4.34 ▲ 1.17% PSSA3 47.92 ▼ 1.60% CVCB3 1.81 ▼ 4.23% POSI3 3.88 ▼ 2.27% SLCE3 17.19 ▼ 0.87% NATU3 9.94 ▲ 1.53% BRKM5 12.21 ▲ 0.49% RANI3 7.85 ▼ 0.25% CSNA3 6.42 ▼ 3.75% CMIN3 4.72 ▼ 1.05% USIM5 9.12 ▼ 7.79% GGBR4 23.34 ▼ 1.02% ENEV3 25.06 ▼ 3.43% NEOE3 33.80 — 0.00% CPFE3 44.52 ▼ 1.53% CMIG4 11.27 ▼ 0.09% EQTL3 38.59 ▼ 0.54% LREN3 13.55 ▼ 1.24% VIVT3 35.52 ▼ 0.20% RAIL3 14.97 ▼ 1.96% KLABIN 16.43 ▼ 2.55% RAIA DROGASIL 19.59 ▼ 0.25% RDOR3 34.84 ▲ 0.26% HAPV3 12.45 ▼ 6.11% FLRY3 15.60 ▼ 2.26% SMTO3 18.25 ▼ 0.82% UGPA3 29.13 ▼ 1.42% VBBR3 33.12 ▼ 0.81% BBSE3 34.12 ▼ 1.04% BPAC11 54.50 ▼ 1.61% CURY3 30.37 ▼ 0.75% AERI3 2.42 ▼ 0.41% VIVARA 22.94 ▼ 0.26% COMPASS 25.90 ▼ 1.89% VAMOS 3.41 ▼ 2.29% SANB11 26.92 ▼ 0.81% ASAI3 8.50 ▼ 1.05% SBSP3 29.03 ▼ 1.66% WALMEX 54.82 ▲ 0.53% GMEXICO 202.10 ▼ 4.45% FEMSA 210.39 ▼ 0.01% CEMEX 21.82 ▼ 3.71% GFNORTE 184.04 ▼ 0.98% BIMBO 59.19 ▲ 0.27% TELEVISA 9.94 ▲ 1.43% AMX 23.13 ▼ 1.11% GAP 413.32 ▼ 1.41% ASUR 296.14 ▼ 1.66% OMA 222.96 ▼ 0.70% KOF 180.84 ▼ 0.13% GRUMA 298.23 ▲ 0.12% KIMBER 38.28 ▼ 0.55% SQM-B 76,590 ▼ 2.06% COPEC 6,145 ▼ 0.08% BSANTANDER 68.99 ▼ 0.16% FALABELLA 5,500 ▲ 1.08% ENELAM 75.75 ▼ 0.89% CENCOSUD 2,060 ▼ 3.06% CMPC 1,055 ▼ 0.94% BANCO CHILE 163.70 ▲ 0.13% LATAM AIR 21.54 ▼ 2.53% YPF 65,000 ▼ 0.46% GGAL 6,060 ▼ 2.02% PAMPA 4,720 ▼ 0.26% TXAR 615.00 ▲ 0.49% ALUAR 940.50 ▼ 0.42% TGS 8,750 ▼ 0.62% CEPU 2,049 ▼ 3.17% MIRGOR 17,225 ▼ 3.23% COME 42.52 ▼ 1.51% LOMA NEGRA 3,105 ▼ 1.82% BYMA 272.25 ▼ 2.77% TELECOM ARG 3,505 ▼ 4.24% ECOPETROL 13.11 ▼ 0.87% BANCOLOMBIA 63.16 ▼ 1.83% GRUPO AVAL 4.01 ▼ 5.20% CREDICORP 316.31 ▼ 3.47% SOUTHERN COPPER 176.78 ▼ 6.22% BUENAVENTURA 34.29 ▼ 7.70% MERCADOLIBRE 1,547 ▼ 3.77% NUBANK 12.19 ▼ 5.72% XP 17.47 ▼ 0.74% PAGSEGURO 8.86 ▼ 1.66% STONE 9.61 ▼ 0.93% GLOBANT 38.87 ▲ 14.06% TECNOGLASS 38.61 ▼ 5.90% GAP AIRPORT 238.45 ▼ 2.15% ASUR 296.14 ▼ 1.66% OMA AIRPORT 102.84 ▼ 1.57% AMX ADR 26.59 ▼ 1.85% FEMSA ADR 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Latin America Sports

Latin America: Earth’s crust under the Andes is sinking -study

By · July 27, 2022 · 3 min read

Geologists have discovered a sinking of the Earth’s crust under the Andes. The study has confirmed that the part under the rock layer is “seeping” deep into the planet, which explains some of the features of the mountains.

Certain parts of the Andes have features that the plate tectonics theory cannot explain. It has long puzzled scientists. Now a team led by geologists at the University of Toronto has found the answer to the riddle: The crust, the Earth’s outermost layer of rock, is sinking beneath these areas.

According to the team, this happens because the part under the crust, the lithosphere, thickens and heats up, causing it to “leak” downward due to gravity.

The central Andes include parts of Peru, Bolivia, Chile, and Argentina.
The central Andes include parts of Peru, Bolivia, Chile, and Argentina. (Photo: internet reproduction)

“Because of its high density, it drips like honey into the deep interior of the planet and is likely responsible for two major tectonic events in the central Andes: changing the surface topography of the region by hundreds of kilometers and flattening and stretching the crustal surface itself,” explains Julia Andersen, lead author of the study published in Communications Earth & Environment.

In this phenomenon, called lithospheric drift, crustal fragments sink into the Earth’s lower mantle. As a result, a basin first forms at the surface, and then the land mass moves upward for hundreds of kilometers. Lithospheric drift has been detected elsewhere on Earth, such as in the central Anatolian Plateau (Turkey) and the Great Basin in the western United States.

WHAT IS HAPPENING IN THE ANDES?

The central Andes include parts of Peru, Bolivia, Chile, and Argentina. This region is bounded by the Puna and Altiplano plateaus and was formed millions of years ago when the Nazca Plate slid under the South American Plate.

However, its unusual features suggest that it was not formed uniformly. The Puna Plateau, for example, is characterized by a higher average elevation and includes several isolated inland basins and volcanic centers.

One of these basins, the Arizaro Basin between Chile and Argentina, “is not defined by known tectonic plate boundaries, suggesting that it is a more localized geodynamic process,” explains Russell Pysklywec, co-author of the study.

The team suspected that lithospheric drip had something to do with it. Previous studies using seismic imagery have detected evidence of this phenomenon in the region but have not directly linked it to what is observed at the surface.

A “GROUNDBREAKING” EXPERIMENT

Andersen and his colleagues set out to recreate in their laboratory what had been happening in this vast region over the past twenty million years.

They developed a three-dimensional model representing the Earth’s layers beneath the central Andes using materials such as sand, clay, and silicon “under incredibly accurate submillimeter measurement conditions,” Andersen said.

First, a tank was filled with polydimethylsiloxane (PDMS), a very thick liquid, to simulate the Earth’s lower mantle. On top of that, a solid mixture of PDMS and clay was applied to represent the upper mantle and lithosphere. Finally, a sand-like layer of ceramic and silica was applied to serve as the Earth’s crust.

The scientists compacted a portion of the clay and PDMS layer (lithosphere), which began to leak downward. “The dripping occurs over hours, so you don’t see much from one minute to the next,” Andersen says. The study presents snapshots every ten hours to show the progress of the trickle.

The team then examined the effects of the trickle on the crustal layer and compared it to the sediment record in the central Andes over millions of years. They found that the changes in crustal height in their model were similar to those in this South American region, particularly in the Arizaro Basin.

“We also observed crustal shortening with folds in the model, as well as basin-like depressions at the surface, so we are confident that a drop is very likely the cause of the observed deformations in the Andes,” Andersen affirms. “These results indicate that the lithosphere may be more volatile or fluid than we thought,” Pysklywec said.

With information from Latina Press

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