Prof. Lizeth Caballero (UNAM) seminars at University of Bari, Italy

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12-12-12-12-12-12-12-12-12-12-12-12



 From: Fabio Dioguardi <fabiodioguardi@xxxxxxxxx>


Dear community,

I would like to invite you to attend the following two seminars given by
Prof. Lizeth Caballero Garcia, Universidad Nacional Autonoma de Mexico
(UNAM), Mexico.

The seminar will take place on the 20th and 22nd January 2025, 15.00 CET at
the Dipartimento di Scienze della Terra e Geoambientali, University of
Bari, Aula 1. The seminar can be attended from remote via Microsoft Teams
using the link provided below.
How to reach us: http://www.geo.uniba.it/dipartimento/come-raggiungerci.html
<https://urldefense.com/v3/__https://aivulc.us13.list-manage.com/track/click?u=575f06dcb490848dc236f67c5&id=3aa34213fa&e=a2c6e925a5__;!!IKRxdwAv5BmarQ!dtBBcy6V_cwT2mgG9OvnP2Q-49_HDhammbZ23v8qFlXF4xLMNevDGMM3R-FAT0UNHlKkz1p0dfltHvXtw-UANfyvjw$>

Title: *Inter-eruptive lahar hazard scenarios associated to low latitude,
ice-capped stratovolcanoes: an example from Pico de Orizaba volcano, Mexico*
20th January 2025 15:00 CET

Inter-eruptive lahars represent a hazard associated with volcanoes that are
not currently in an eruptive state.  In the last years, they have occurred
at Pico de Orizaba due to the availability of loose material, extreme
climate conditions favoring certain weathering- and erosion processes, as
well as triggers being mostly extreme precipitation events. Moreover, the
glacier retreat that has occurred over the past few decades has resulted in
the exposure of loose material that is susceptible to being mobilised,
thereby increasing the likelihood of lahars and other mass movements.  As
glaciers recede, they can become a source of water themselves. However,
they can also become unstable, as has been observed in mountainous regions.
In this seminar, I will discuss the upper slope conditions at Pico de
Orizaba volcano, as well as the trigger conditions of previous
inter-eruptive lahars within the glacier-influenced basins at this volcano.
Microsoft Teams link
<https://urldefense.com/v3/__https://teams.microsoft.com/l/meetup-join/19*3ameeting_NDI2MDMyYzQtZmZmZS00YjMyLWJiNTUtYzA0NWZmNjE4YjVi*40thread.v2/0?context=*7b*22Tid*22*3a*22c6328dc3-afdf-40ce-846d-326eead86d49*22*2c*22Oid*22*3a*226f9d5ef7-a702-4e54-aae0-32f468d91c8b*22*7d__;JSUlJSUlJSUlJSUlJSUl!!IKRxdwAv5BmarQ!dtBBcy6V_cwT2mgG9OvnP2Q-49_HDhammbZ23v8qFlXF4xLMNevDGMM3R-FAT0UNHlKkz1p0dfltHvXtw-X3taMwQA$>

Title: *Hazard assessment for secondary lahars at Atitlán-Tolimán Volcanic
Complex (Guatemala)*
22nd January 2025 15:00 CET

The Atitlán and Tolimán volcanoes are part of the Central American Volcanic
Arc and are located on the southern edge of the Atitlán caldera. They are
two neighboring volcanoes, aligned north-south, whose drainage network is
integrated. Tolimán volcano has not exhibited any eruptive activity during
the Holocene epoch. In contrast, Atitlán, the youngest volcano, has it last
confirmed eruption in 1856. Despite the absence of recent volcanic
activity, three disasters have occurred in the area since 2000. These
events occurred in 2002, 2005, and 2010, respectively, and were caused by
the formation of lahars triggered by rainfall. The lahars resulted in the
burial of the towns of El Porvenir, Panabaj, and Pampojilá. In light of
these events, the project "Warning and monitoring system for volcanic
eruptions in Guatemala and disseminated in Central America" developed a
lahar hazard map for this volcanic complex. The map and associated products
represent the outcome of a multinational and inter-institutional
collaboration between INSIVUMEH, CONRED, and the Vivamos Mejor Association
(Guatemala), in conjunction with UNAM (Mexico), and funded by the Swiss
Cooperation of Central America. These tools are fundamental for
comprehensive risk management and disaster risk reduction in Guatemala.
Microsoft Teams link
<https://urldefense.com/v3/__https://teams.microsoft.com/l/meetup-join/19*3ameeting_YTY5ZjRlNzUtNTc3Mi00ZTU4LWJjNjAtOGI2MmUzMGE5YzIz*40thread.v2/0?context=*7b*22Tid*22*3a*22c6328dc3-afdf-40ce-846d-326eead86d49*22*2c*22Oid*22*3a*226f9d5ef7-a702-4e54-aae0-32f468d91c8b*22*7d__;JSUlJSUlJSUlJSUlJSUl!!IKRxdwAv5BmarQ!dtBBcy6V_cwT2mgG9OvnP2Q-49_HDhammbZ23v8qFlXF4xLMNevDGMM3R-FAT0UNHlKkz1p0dfltHvXtw-UsAPw0iw$>

For further information: Dr. Fabio Dioguardi, fabio.dioguardi@xxxxxxxx





12-12-12-12-12-12-12-12-12-12-12-12



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