Trace Fossil
Moraines are formed by the deposition of glacial debris as a glacier moves and erodes the land. As the glacier melts, it leaves behind ridges and mounds of unsorted sediment. The size and shape of a moraine can vary depending on the glacier's movement and the type of sediment deposited.
A canyon is a landform that is typically formed by erosion, often from the movement of sediment-laden water like a river. Erosion gradually wears away the rock or land surface, carving out a canyon over time.
Rocks formed from sediment deposits are called sedimentary rocks. They are formed from the accumulation and lithification of sediment, which can include fragments of pre-existing rocks, minerals, and organic material. Examples include sandstone, shale, and limestone.
A glacier formed Long Island which came from Canada
Erosion is the process in which sediment moves from one location to another.Do not get this confused with deposition, which is the process in which sediment is dropped (deposited) in a new location.
Coprolites are formed when feces get buried and are preserved over time by mineralization. As the feces become compacted and fossilized, they turn into coprolites. The minerals in the surrounding sediment replace the organic material, leaving behind a fossilized record of the animal's diet and digestive system.
Fossilized coral is brought to the Earth's surface primarily through geological processes such as tectonic uplift and erosion. Over millions of years, coral reefs that formed in ancient seas can become buried under sediment and subsequently uplifted by the movement of tectonic plates. Erosion over time removes overlying materials, exposing these fossilized remains. Additionally, changes in sea levels can contribute to the exposure of coral fossils as landmasses shift.
The fossilized ripples tell us about the environmental conditions when the rock was formed
Fossilized tree sap is called amber.-Leah Ward
Fossilized monkey puzzle tree.
Coal.
It was formed by sediment
Dragonfly fossils are formed through a process called fossilization, where a deceased dragonfly would typically be buried in sediment or mud. Over time, the soft tissues decompose, leaving behind hard parts such as exoskeletons or wings that can become fossilized. The surrounding sediment eventually hardens into rock, preserving the dragonfly remains as a fossil.
coal
mold
Burrows - formed by organisms digging or tunneling in sediment. Trackways - impressions left by animals walking or moving across a surface. Coprolites - fossilized feces of animals. Bioturbation - disturbance of sediment by biological activity. Borings - holes or tunnels made by organisms drilling into hard surfaces.
Fossils are formed when organisms are buried quickly after death, typically in sediment such as mud or sand, which protects them from decay and scavengers. Over time, minerals seep into the remains, gradually replacing organic material and creating a rock-like replica. For example, a dinosaur bone can become a fossil if it is buried in sediment, where it undergoes mineralization over millions of years, eventually turning into a hard fossilized bone.