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  2. Lázaro Cárdenas - Wikipedia

    en.wikipedia.org/wiki/Lázaro_Cárdenas

    Šetalište Lazaro Kardenasa (Lázaro Cárdenas promenade) in Belgrade, Serbia, is also named after him, as is a street in Barcelona, Spain, and a monument in a park in Madrid dedicated to his memory for his role in admitting defeated Spanish Republicans to Mexico after the Civil War in that country. In Chicago, Lazaro Cardenas K-8 School in ...

  3. Lázaro Cárdenas, Michoacán - Wikipedia

    en.wikipedia.org/wiki/Lázaro_Cárdenas,_Michoacán

    It was formerly known as Los Llanitos, but changed its name as a tribute to Lázaro Cárdenas del Río, a Michoacán-born politician who was president of Mexico from 1934 to 1940. The city's coordinates are 17°57′00″N 102°12′00″W  /  17.95000°N 102.20000°W  / 17.95000; -102.20000 , where the Río Balsas drains into the Pacific

  4. Mexican president-elect taps heir of leftist icons as her ...

    www.aol.com/news/mexico-president-elect...

    MEXICO CITY (Reuters) -Mexican President-elect Claudia Sheinbaum announced on Thursday that she has chosen Lazaro Cardenas, a former congressman and governor and a scion of two of Mexico's most ...

  5. 1934 Mexican general election - Wikipedia

    en.wikipedia.org/wiki/1934_Mexican_general_election

    General elections were held in Mexico on 1 July 1934. The presidential elections were won by Lázaro Cárdenas, who received 98% of the vote. [1] Results.

  6. Los Pinos - Wikipedia

    en.wikipedia.org/wiki/Los_Pinos

    Los Pinos (English: The Pines) was the official residence and office of the President of Mexico from 1934 to 2018. Located in the Bosque de Chapultepec (Chapultepec Forest) in central Mexico City, it became the presidential seat in 1934, when Gen. Lázaro Cárdenas became the first president to live there.

  7. Lázaro Cárdenas, Quintana Roo - Wikipedia

    en.wikipedia.org/wiki/Lázaro_Cárdenas,_Quintana...

    Like most of the Yucatan Peninsula, Lázaro Cárdenas is entirely flat with a gentle slope towards the sea, so from west to east.. Like the rest of the peninsula's surface, the land has a limestone base that does not allow the formation of surface water flows such as rivers and streams, the water instead forms flows in underground rivers that sometimes rise to the surface in the cenotes.

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