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The Baribis Fault (Indonesian: Sesar Baribis) is a geological feature located in the northern part of Java. [1] This fault, estimated to be 100 kilometers (62 miles) long, stretches from Purwakarta to Lebak Regency [2] and is a threat to the Jakarta metropolitan area because the fault is partially located within the metropolitan area itself.
The bleeding may be due to placental abruption, uterine rupture, placenta accrete, undiagnosed placenta previa, or vasa previa. [3] Cesarean section is indicated. Post-partum hemorrhage is defined by the loss of at least 1,000 mL of blood accompanied with symptoms of hypovolemia within 24 hours after delivery.
The Lembang Fault (Indonesian: Sesar Lembang) is an active fault located 10 km north of the city of Bandung on the Indonesian island of Java.This sinistral slip fault is estimated to measure 29 km in length. [1]
The SESAR 3 JU is co-funded by the European Union through the Horizon Europe research and innovation programme and industry as follows: • Horizon Europe - EUR 600 million • Eurocontrol – up to EUR 500 million (in-kind and financial contributions) • Industry - EUR 500 million minimum (in-kind and financial contributions) In addition, the Digital European Sky programme will benefit from ...
Non-specific immunity results in no immunologic memory. There are mechanical, chemical, and biological factors affecting the effectiveness and results of the non-specific immune response. These factors include the epithelial surfaces forming a physical barrier, fatty acids that inhibit the growth of bacteria, and the microflora of the ...
2004: SESAR definition phase started. June 2008: SES-II regulation adopted. 8 December 2008: inauguration of the SESAR Joint Undertaking. 3 June 2009: official start of the SESAR development programme. 12 June 2009: SESAR Joint Undertaking signs agreement with 16 partners totalling €1.9 billion for the creation of the Europe's future ATM system.
A 3-metre (9.8 ft) tsunami caused moderate damage to the port and airport facilities on Simeulue, and a 2-metre (6.6 ft) tsunami was recorded on the west coast of Nias. [21] Much smaller waves, most detectable only in tide gauge recording systems, were recorded across the Indian Ocean; for example, a 0.21m wave was recorded at Colombo , Sri Lanka .