Updates on Earthquakes for Feb 6th Feb 12th and Updates on the Channel

Huatulco Food Bank

https://www.paypal.me/rlclearwater

Mexico's poverty rate declines from 50% to 43.5% in four years as remittances almost double. MEXICO CITY The poverty rate in Mexico has declined from 49.9% of the population in 2018 to 43.5% in 2022, according to a study published Thursday by the country's poverty analysis agency.

James Wright

PO Box 795 PIE TOWN NM 87827

EMAIL deeptruthdeepimpact@yahoo.com

Telegram it's a great place to meet and put up your links, that you consider is very important and basically to touch base with the family over there so many are doing great work on Telegram with the links

FINE TELEGRAM

Earth Changes News Channel 🌎 Chat Room

THE NEW LINK https://t.me/+9phDoj65mORjMjlh

Tectonic setting and earthquakes

Greece is located at the complex boundary zone in the eastern Mediterranean between the African plate and the Eurasian plate. The northern part of Greece lies on the Eurasian plate while the southern part lies on the Aegean Sea plate.
The Aegean Sea plate is moving southwestward with respect to the Eurasian plate at about 30 mm/yr while the African plate is subducting northwards beneath the Aegean Sea plate at a rate of about 40 mm/yr.
The northern plate boundary is a relatively diffuse divergent boundary while the southern convergent boundary forms the Hellenic

These two plate boundaries give rise to two contrasting tectonic styles, extension on east–west trending fault zones with strike-slip tectonics on SW-NE trending fault zones throughout west and central Greece, Peloponnese and the northern Aegean and contractional in the southern Aegean, continuing around to the Ionian Islands.
The south Aegean is the location of the volcanic arc and is characterized by extension. To the east of Crete along the Hellenic Arc, strike-slip tectonics with some extension become important.

The strongest earthquakes historically are those associated with the Hellenic Arc, although none larger than about 7.2 have been observed instrumentally. The events of AD 365 and 1303 are likely to have been much larger than this. In mainland Greece, normal faulting gives earthquakes up to 7 in magnitude, while in the northern Aegean, strike-slip events with a magnitude of 7.2 have been recorded. Large intermediate depth (>50 km) earthquakes of magnitude >7 from within the subducting African plate have been recorded but such events cause little damage, although they are widely felt.