Summit and Crater:
* Summit: The highest point of the volcano, currently marked by the "Pelée's Needle" (a spire of solidified lava).
* Crater: The opening at the top of the volcano where volcanic material is ejected. This is where the "Pelée's Needle" formed after the 1902 eruption.
Cones and Domes:
* Morne Macouba: A parasitic cone on the southwestern flank of Mount Pelée.
* Morne Jacob: Another parasitic cone located on the northern flank.
* Lava Domes: These are formed by the slow extrusion of viscous lava, which cools and solidifies within the crater or on the volcano's flanks.
Flank Features:
* Pyroclastic Flows: These are fast-moving currents of hot gas and volcanic debris, which traveled down the flanks of the volcano during past eruptions.
* Lahars: Volcanic mudflows, often triggered by heavy rainfall or eruptions, which flow down the volcano's slopes.
* Lava Flows: Streams of molten rock that flowed down the volcano's flanks during eruptions.
Other Notable Features:
* The "Pelée's Needle": A towering spire of solidified lava, formed after the 1902 eruption. This spire collapsed in 1905.
* The "Prêcheur Valley": The valley located on the southwestern flank of Mount Pelée, which was devastated by the 1902 eruption.
Remember: The features of volcanoes are constantly evolving as new eruptions occur, shaping and reshaping the landscape. The above description provides a general understanding of the parts of Mount Pelée, but it's important to consider the dynamic nature of volcanoes.
