πŸ– Rift PTS Datamining – February 25, – Enclave of Ahnket and more – The Ghar Station

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(b) The interferogram for the May dyke intrusion at the Manda Hararo rift segment. ) and Alu-Dalafilla in , and followed by the eruptions of Erta Ale in in the Red Sea Rift of Northern Afar. Article. Full-text available. Mar


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Rifts and rifted margins worldwide show a large structural variety as a result of the interaction of rock occurred in Afar: the Alu-Dalafilla eruption in continental margin of Norway 4, years ago, Geo-Mar Lett,. 22(1).


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∼12 km beneath Alu-Dalafilla at the rift axis. Accepted article online 1 MAR () propose that the WSW dipping faults of the mar-.


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crustal magma chambers beneath the central rift valley (e.g., Main Ethiopian, Afar​, and Eastern or strata deposited near or below sea level on the two passive mar- gins record eruption of Alu-DallaFilla in northern Afar, accompanied.


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Google Maps screen capture. Image courtesy Acocella, et al, Since this is my first excursion into the Afar Triangle, a short discussion of the region is in order. Climate is generally hot and dry with cooler desert nights. These eruptions coincided with regional uplift of the Ethiopian plateau. These segments are typically parallel separated by a couple kilometers. There is an extensive hydrothermal system associated with the rifting volcanism. Surveys of the region discovered active fumaroles, hot springs on the sedimentary plains, and gas emissions from several sites surrounding the fissure system. Note that the plateau is a combination of uplift and basalt deposits from the Afar flood basalt. Total coverage of these basalts was , km2 on the Africa side of the combined rifts. There have been three small volume basaltic eruptions from the southern and central parts of the axial graben in , and These fissure eruptions produced rubbly pahoehoe flows up to 2 m thick. A paper by Haga, et al described field studies necessary to exploit the Manda β€” Inakir rift system for geothermal energy. Rift volcanism at the southern Manda Haro Rift. This volcanic activity is similar to that along mid-oceanic ridge segments. The older Inakir rift has volcanic rocks overlying a NW β€” SE dome 12 x 25 km cut by a 2 β€” 3 km wide rift zone. The dike was detected via seismicity and surface deformation. The Kammourta volcano is flagged at the red pointer. Manda β€” Inakir was the site of a β€” basaltic eruption that created a cinder cone and lava flow near the village of Korili and the Andabba Plain. Volcanic activity here is concentrated along two parallel rifts, Manda and Inakir. Multiple lava flows at center to the south of the main line of lava flows is the Dabbahu Manda Hararo rifting event of β€” The Andabba plain is to the lower right of the image. Dike volume was 2. The Dabbahu β€” Manda Hararo activity β€” is the most recent volcanic activity associated with rifting propagation. The Manda β€” Inakir range has two rift zones. Image courtesy Wadge, et al, The Mousa Ali stratovolcano sits on the tri-point intersection of the Ethiopia, Djibouti and Eritrea borders. There are similarities to the relationship between fissure swarms and central volcanoes also seen in Iceland. Kammourta marks the SE location of the Manda β€” Inakir rift. The triple junction for all these tectonics is the Afar, which has the Ethiopian Plume head underneath it, providing copious amounts of eruptible magma. Image courtesy Google Maps screen capture. In addition to the Large Igneous Province event 31 β€” 29 Ma, there have been multiple volcanic episodes in the Afar. This propagation has been driven by what is called the Ethiopian Plume Head, a hotspot that arrived around 30 Ma. Image courtesy Beccaluva et al, Recent activity in the Afar are located along axial grabens along the rifting segments, and include fissure eruptions, silicic central volcanoes and basaltic shield volcanoes. Rift propagation is also noted along with relative movement along major rifts. Central volcanic centers produce basalts while marginal volcanic centers produce trachyites, rhyolites and ignimbrites. Total volume of these traps is estimated at 1. The Stratoid Series is a pile of 1 β€” 6 thick pahoehoe basalt flows up to 1, m thick on the floor of the Afar Depression. Schematic of recent volcanic activity in the Afar. Since this began in , there have been 13 basaltic dikes emplaced. Hydrothermal system and wells surrounding Manda β€” Inakir. In short, the region is a tectonic mess, as a triple junction of rifts propagates W to SW into Africa. Red rounds are fumaroles. Double circles are water wells. It is 2, m high, topped with a caldera, and rhyolite lava domes and flows. Proposed schematic of mantle plume underlying the Afar and Ethiopian Plateau. The region is part of an active seafloor rifting event that is part of the Afar Depression. The plume head arrival created the most recent Large Igneous Province eruption sequence in the Afar with basalt eruptions peaking some 30 Ma. The SE end of this rift moved inland and continues to rift in roughly 60 km long segments. Manda Inakir should be similar in nature.

Manda β€” Inakir recent volcanism. Image courtesy Dumont, et al, The region is rift alu mar to click here Ethiopian β€” Djibouti border in the Ethiopian highlands. This rifting event opened a series of rift alu mar and rift alu mar faults along a 60 km segment of the rift.

Note the Afar depression and the rift in the plateau. Lava flows are depicted in purple. Image courtesy Smithsonian GVP. Though there is a proposed geothermal project on the Djibouti side of the border based on the presence of magma relatively close to the surface.

Manda Hararo rifting event. Satellite view of β€” Manda Hararo rifting lava flows. The activity began in September with a large dyke emplacement. Image courtesy Maguire, et al, Overall tectonic movement has been movement of the Arabian Plate away from Rift alu mar, opening the Red Sea.

Blue squares are hot springs. Crust thickness of this part of the Afar varies from around 16 km to the north and 45 km beneath the Ethiopian plateau.

The Wiki describes its vegetation as lush with flowering shrubs and plants. The more recent Manda rift has roughly the same orientation, parallel with the Https://agency-people.ru/2020/2020-home-lottery-winners.html rift.

Initial research into geothermal potential of the region suggests it can support a number of micro-geothermal plants in the 10 β€” kW range.

The region is economically poor, with little infrastructure. In some ways, volcanic activity has been nearly continuous for the last 4 Ma in the Afar.

Activity in Yemen covered at least 80, km2. The northern portion of this active region is defined by the propagation of rifting under the Red Sea.

Propagation of Red Sea rift into the Manda β€” Inakir region. Recent eruptions located via red stars. The older Inakir rift had volcanic rocks overlying an 12 x 25 km dome of basement world series of poker champion 2020.

That end is 2 km wide and fractured. It is the β€” most recent eruption from this system. The Manda β€” Inakir activity is at the SW end of this rifting segment. Well depths would be in the 1 β€” 2 km range. It projects into Ethiopia with only the southern end in Djibouti. There is a volcanic edifice located right at the triple junction between the three national borders, Ethiopia, Djibouti and Eritrea. The Ethiopian plateau has been lifted at least 2 km by the underlying mantle plume. It is a smallish volcanic eruption NW of the Ethiopia β€” Djibouti border. This vegetation supports abundant wildlife. Active fissure eruptions. The location of the most recent eruption in β€” is a full m above sea level in Djibouti near the SE end of the rifts. Image screen capture from Haga, et al. It is perhaps 10 km to the NE of the Manda β€” Inakir volcanic rifts. Orange rounds are gas emissions with bubbling water sounds. Granyia did an excellent post on Ardoukoba November We will use the Manda β€” Inakir as a starting point for the larger discussion of recent volcanism in the region. Trees and local forests tend to be located where local water pools. Ran across this one via Smithsonian GVP. Afar and Yemen flood basalts on Ethiopian Plateau. There was a small rhyolite eruption from a fissure at the northern tip of the dike. Drilling for local water wells has discovered what is described as anomalous hot water occurrences, with occasional temperatures above 80 C. Its most recent eruption was perhaps , years ago. The Ethiopian trap basalts were erupted 31 β€” 29 Ma.