Thousands of Venezuelan families are living in public squares, streets, and vehicles after twin earthquakes destroyed their homes on June 24, 2026 [3].
The crisis highlights a growing humanitarian emergency in the capital, where the lack of adequate government assistance has forced displaced citizens to create improvised refugee camps in urban centers.
The disaster began with two powerful seismic events on June 24, 2026 [3]. The first earthquake measured 7.2 magnitude, followed by a second quake reaching 7.5 magnitude [1]. These events rendered countless homes unsafe or completely destroyed them, leaving residents with no choice but to migrate to open spaces.
In Caracas, the displacement is most visible in seven major plazas [4]. Families have established makeshift shelters in Plaza Altamira, Moneda, Juventud, Morelos, Panteón Nacional, Darío Vivas, and Parque Carabobo [2]. These public spaces, along with sidewalks and parks, now serve as primary residences for those who have lost everything.
Beyond the capital, similar scenes are unfolding in Guaira, located in the state north of Caracas [2]. Many displaced people are sleeping in their cars or under trees, facing uncertainty about where they will live in the coming months [2].
Residents said that government aid has been insufficient to meet the scale of the need [1]. This gap in support has turned the city's infrastructure into a sprawling network of temporary camps. Families continue to occupy these public spaces as of this week, struggling to find permanent housing solutions while living exposed to the elements.
“Families have established makeshift shelters in seven major plazas in Caracas.”
The transition of public plazas into long-term refugee camps indicates a systemic failure in disaster response and urban resilience. By relying on improvised shelters in the heart of Caracas, the displaced population is not only facing a housing crisis but is also creating a permanent visible marker of the state's inability to provide basic emergency infrastructure following high-magnitude seismic events.
