geosciences Article Seismically Induced Soil Liquefaction and Geological Conditions in the City of Jama due to the M7.8 Pedernales Earthquake in 2016, NW Ecuador Diego Avilés-Campoverde 1,*, Kervin Chunga 2 , Eduardo Ortiz-Hernández 2,3, Eduardo Vivas-Espinoza 1, Theofilos Toulkeridis 4 , Adriana Morales-Delgado 1 and Dolly Delgado-Toala 5 1 Facultad de Ingeniería en Ciencias de la Tierra, Escuela Superior Politécnica del Litoral, Campus Gustavo Galindo Km 30.5 Vía Perimetral, P.O. Box 09-01-5863, Guayaquil 090903, Ecuador;
[email protected] (E.V.-E.);
[email protected] (A.M.-D.) 2 Departamento de Construcciones Civiles, Facultad de Ciencias Matemáticas, Físicas y Químicas, Universidad Técnica de Manabí, UTM, Av. José María Urbina, Portoviejo 130111, Ecuador;
[email protected] (K.C.);
[email protected] (E.O.-H.) 3 Department of Civil Engineering, University of Alicante, 03690 Alicante, Spain 4 Departamento de Ciencias de la Tierra y de la Construcción, Universidad de las Fuerzas Armadas ESPE, Av. Gral. Rumiñahui s/n, P.O. Box 171-5-231B, Sangolquí 171103, Ecuador;
[email protected] 5 Facultad de Ingeniería, Universidad Laica Eloy Alfaro de Manabí, Ciudadela Universitaria, vía San Mateo, Manta 130214, Ecuador;
[email protected] * Correspondence:
[email protected] Abstract: Seismically induced soil liquefaction has been documented after the M7.8, 2016 Pedernales earthquake. In the city of Jama, the acceleration recorded by soil amplification yielded 1.05 g with an intensity of VIII to IXESI-07. The current study combines geological, geophysical, and geotechnical Citation: Avilés-Campoverde, D.; data in order to establish a geological characterization of the subsoil of the city of Jama in the Manabi Chunga, K.; Ortiz-Hernández, E.; province of Ecuador.