Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Pico Bonpland

Structural and Tectonic Formations

Pico Bonpland is Venezuela's fourth-highest peak, rising to 4,883 metres in the Sierra Nevada de Merida of the Venezuelan Andes in Merida State. Named for the naturalist Aime Bonpland, who never actually visited the Venezuelan Andes, the peak and its neighbor Pico Humboldt are protected within Sierra Nevada National Park. Glaciers formed on Pico Bonpland during the Pleistocene-era Merida glaciation had entirely disappeared by 2011. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Pico Bonpland

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Pico Bonpland
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Also in Geography Atlas: where this subject is found.

Source Wikidata: Pico Bonpland
Sources
1. Pico Bonpland (Wikipedia)
Lead section
Quote, Lead section
The peak with its sister peak Pico Humboldt, and the surrounding páramos are protected by the Sierra Nevada National Park.
View the Source
Wikidata: Pico Bonpland
Wikidata Q3646551, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.