... landscape was increasing ( Table 6.1 ) . In the second half of the twentieth century , the cultural landscape in the Moravian - Silesian Carpathians experienced essential changes and geomorpho- logical processes were accelerated . After ...

... landform assemblages (Table 2.3). Only the predictions of gneisses and schists were correct or partly correct ... landform criteria were difficult to employ because similar landforms are ascribed to different rock types. Thus, both ...

... landform easier. A sloperaster was derived from the 50m contour lines to ... landform polygons representing similar physiography. Contour lines of Digital ... Table 1 shows the landform types identified by the MEDSCAPES protocol, their ...

... Table 1. Pre - Tertiary structural units ( basin basement ) of Hungary / 23 Table 2. Genetic classification of the polygenetic geomorphic surfaces of planation of the Transdanubian horst - series / 32 Table 3. Major changes of climate ...

... landform classb Profile curvature Plan curvature 1 concave 6 , 7 convex convex 1 concave 7 ; separates 3 , convex 5 from 4 3 7 FIGURE 5 long SW-facing slope, trending NW from the Northern. TABLE 2 Landform classification based on TPI ...

... (Table 6.1). The Harbours' 'multi-finger' creeks (Table 6.2) possess a longer inland incision than their 'glove-finger' (Table 6.3) counterparts further to the north. Of particular importance is the distinction between 'glove-finger' and ...

... table is shown in Figure 11. Units in column 6 show the names of the classification units assigned to the geoform ... Landform classes were converted to CMECS geoforms primarily by re-naming them as appropriate for the marine setting in which ...

... Table 2.7. A total of 560, 567, 530, and 414 drillings were found in the Shenmu–Mizhi, Suide–Yanchuan, Yanan–Yanshui, and Tongchuan–Huangling highways, respectively (Table 2.8). The geophysical prospecting profiles were detected by ...

... landscape, and profile concavity is more common at low altitudes. Table 3 shows that the linear correlation between profile convexity and altitude is always positive, but usually quite weak. It rises above +0.5 only for single landforms ...

... (Table 10.5) (Comănescu et al. 2011b). “The scientific value scores well too as these geomorphosites are vital in understanding the genesis and evolution of the glacial relief in this area” (Comănescu et al. 2011b). The scores vary ...