some fossils of shell and fish have been found at the top of the rocky mountain peaks. How do you suppose this happen?
Shells on mountains are easily explained by uplift of the land. Although this process is slow, it is observed happening today, and it accounts not only for the seashells on mountains but also for the other geological and paleontological features of those mountains. The sea once did cover the areas where the fossils are found, but they were not mountains at the time; they were shallow seas.
When Noah's Biblical flood covered the tops of every mountain peak it left sea creatures and sea shells all over earth.
its really easy people
maybe there was a river
The presence of fossils of shells and fish at the top of the Rocky Mountain peaks can be explained through a geological process known as uplift. Uplift refers to the vertical movement of Earth's crust, causing rocks and geological features to rise to higher elevations over millions of years.
Here is how the process likely occurred:
1. Deposition: The area where the Rocky Mountains are located was once covered by a large inland sea, known as the Western Interior Seaway, during the Late Cretaceous period, which lasted from approximately 100 to 66 million years ago. Over time, sediments containing shells and fish remains settled at the bottom of the sea.
2. Tectonic activity: The Rocky Mountains formed due to the collision of tectonic plates. Around 70 to 50 million years ago, the North American Plate and the Pacific Plate collided, resulting in intense folding, faulting, and uplifting of the Earth's crust. As a result, the sediments and rocks containing fossils were uplifted along with the mountains.
3. Erosion: Subsequent erosion, mainly due to the action of wind, water, and ice, gradually wore away the overlying layers of rocks, exposing the layers containing the fossil remains at higher elevations.
Today, we find fossils of shells and fish at the top of the Rocky Mountain peaks as a result of this geological history. These fossils serve as evidence of the sea that once covered the region and the subsequent tectonic forces that shaped the landscape.