Which natural feature is primarily found in Gros Morne National Park, resulting from geological uplift?

The presence of Tablelands in Gros Morne National Park is a significant result of geological uplift, particularly the exposure of ancient ocean floor material due to tectonic activity. This area showcases a unique landscape formed from rock types that are not typically found at such elevations, including peridotite.

The Tablelands offer a rare glimpse into the processes of plate tectonics, illustrating how the earth's crust can be pushed and contorted over millions of years. This geological feature is noteworthy because its formation is directly linked to the collision between the North American and Eurasian tectonic plates, which has led to the uplift of these rocks that were once part of the ocean floor.

This national park, designated as a UNESCO World Heritage site, is one of the best places to study the impacts of geological forces and offers stunning views reflective of its unique geological history. The distinctiveness of the Tablelands sets them apart from other natural features mentioned, such as valleys, waterfalls, or forests, which can emerge from different geological processes or ecological conditions.