What geological factor can artificially inflate the perceived density of woolly rhino fossils in specific locations?
Answer
River valleys and floodplains concentrating remains over time
While the overall range of the woolly rhino was vast, interpreting the density of skeletal finds requires careful geological consideration because depositional processes can create biases. Specifically, locations like river valleys and floodplains historically acted as natural traps or collection points. Over geological time, water flow concentrates scattered remains, leading to a high density of bones being found there today. Therefore, a location showing a high count of fossils might reflect an ancient river course that effectively trapped remains, rather than necessarily indicating that this specific spot was the absolute center of the most numerous ancient populations.

Related Questions
What environment characterized the woolly rhinoceros's main habitat during the Pleistocene epoch?What unique preservation quality do Siberian finds of *Coelodonta antiquitatis* offer compared to skeletal fossils elsewhere?Which geographical areas mark the approximate western extent of the woolly rhino's Ice Age range?What specific characteristic made the 2007 carcass discovery in northeastern Siberia highly valuable for study?What geological factor can artificially inflate the perceived density of woolly rhino fossils in specific locations?Which museum collection houses a significant woolly rhino femur believed to have originated from Russia?What is the comparison drawn between the evidence provided by Western Europe versus Siberia for the woolly rhino?Which concept is used to describe the primary ecological role of the woolly rhinoceros in its environment?Where does modern data aggregation, like that from GBIF, generally show the concentration of recorded woolly rhino occurrences?What differentiates the locations where woolly rhinos were *living* during the Pleistocene from locations where fossils are *found* today?