A difference in the erosion rate between the equator and the poles of a factor of a few could explain the latitudinal variation in Titan's crater population.
The difference in the erosion and deposition patterns between these two scenarios provides very helpful information in the investigation of historical tsunamis through tsunami deposits.
Because these are detrital grains and not bedrock, we can be confident that this pattern is not a preservation issue linked to the removal of old material from the metamorphic rocks in the Greater Himalaya themselves but represents a real difference in the erosion history along the mountain chain.
Is it possible that some other factor rather than the life-cycle length was responsible for the differences in synteny erosion with the walnut genome among the six investigated genomes?
The different results from the studies mentioned, and the fact that one third of the individuals in the present study did not show any erosive lesions despite regular vomiting, might be explained by individual differences in the susceptibility to erosion.
The results indicate (1) perturbation in the drainage network caused by differences in the resistance to erosion of outcropping lithological units and (2) hillslopes affected by large landslides, earth flows, and rock falls directly reaching the stream bed.
After adjusting for potential confounders, we found no significant differences in the rates of erosion progression between patients taking an alternative anti-TNF agent and patients taking RTX.
In this study, US revealed synovitis more frequently in MCP and PIP joints and bone erosions less frequently in PIP joints in the RA group than in the PsA group, whereas Fournié and colleagues [ 13] reported minimal differences in the amount of erosion and synovitis in MCP and PIP joints of PsA and RA patients.
Therefore, even though a significant difference in the soil erosion rates and fractal dimensions of topographic surface values could be found between the bank gully heads and upstream areas, the temporal variation in the morphological characteristics of bank gully heads was similar to those observed in upstream areas where ephemeral gullies developed.
To further characterize the macroscopic differences in tissue erosion and remodeling among the four groups, sagittal histologic sections from sites known to be involved (medial femoral condyle and patellar groove) were stained with Safranin O. Typical images (selected from n = 5 mice per group) for the treadmill-only and the OA groups are shown in Figure 6.
