What major feature characterized the formation of Kenorland?

The formation of Kenorland, which occurred during the Neoarchean era, is primarily characterized by extensive volcanic and igneous activity. This period was marked by significant tectonic processes that brought together some of the Earth's first continental masses through volcanic activity, leading to the creation of one of the earliest supercontinents.

The environment during the formation was dominated by the processes that could generate large volumes of magma, resulting in vast stretches of volcanic rock that contributed to the assembly of landmasses. The igneous activity not only played a crucial role in the initial formation of Kenorland but also influenced its geological characteristics, including the composition and structure of the continental crust.

Understanding this aspect is key to recognizing how early continental formations were shaped and the dynamic nature of Earth's geology at that time. Other processes such as fragmentation or significant glacier formation occurred at different times in Earth's history and were not defining features of Kenorland's formation.