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Line 235: − − <gallery mode=packed heights=300px widths=300px> − UGM_Mapping_Fig_4.png − UGM_Mapping_Fig_5.png − UGM_Mapping_Fig_6.png − UGM_Mapping_Fig_7.png − UGM_Mapping_Fig_8.png − </gallery>
→Post-mapping stage (reading a geologic map)
==Post-mapping stage (reading a geologic map)==
==Post-mapping stage (reading a geologic map)==
<gallery mode=packed heights=300px widths=300px>
UGM_Mapping_Fig_4.png|V Rules (Derived from Sukandarumidi, 2011)
UGM_Mapping_Fig_5.png|Geomorphology Map (Source : Geologic Mapping Archive)
UGM_Mapping_Fig_6.png|Traverse Map (Source : Geologic Mapping Archive)
UGM_Mapping_Fig_7.png|Geologic Map (Source : Geologic Mapping Archive)
UGM_Mapping_Fig_8.png|Geologic Profile (Source : Geologic Mapping Archive)
</gallery>
After collecting geological data (such as lithology, geological structure, and geomorphology) from field observation, the next step that should be done is the poster which consists of points of observation’s map, geological map, geomorphological map, stratigraphic column, geological history, and photos and diagrams from petrography, paleontology and structural geology analysis. Those data and maps should represent your field geologically.
After collecting geological data (such as lithology, geological structure, and geomorphology) from field observation, the next step that should be done is the poster which consists of points of observation’s map, geological map, geomorphological map, stratigraphic column, geological history, and photos and diagrams from petrography, paleontology and structural geology analysis. Those data and maps should represent your field geologically.
#* This rule is also not applicable in a field that has igneous and metamorphic rocks.
#* This rule is also not applicable in a field that has igneous and metamorphic rocks.
# To make cross sections, we need to make a line for a cross section which will show the appearance of the distribution of all rock units in the field and also the geological structure. Usually, the direction of the cross section is from north to south with a low or steep dip.
# To make cross sections, we need to make a line for a cross section which will show the appearance of the distribution of all rock units in the field and also the geological structure. Usually, the direction of the cross section is from north to south with a low or steep dip.
==Conclusion==
==Conclusion==