|
|
Students' questions about geological map
Flašar, Jan ; Hanus, Martin (advisor) ; Matějka, Dobroslav (referee)
The analysis of student-generated questions (SGQ) is a method to investigate the way of understanding and solving a problem. The style, frequency, type, etc. of the questions can help analyze the target topic, but we can also study differences in understanding and way of thinking among individual groups of respondents. This study was focused on the analysis of the questions generated by high school students working with the geological map of the Czech Republic and the local geological map (map of Prague). The main goal of this study was to find out whether the questions generated by students differ between individual groups of respondents (according to their age, gender, grade, etc.) and whether they differ for individual types of maps. The questions obtained were classified into categories and the frequency of questions in different categories was determined. Furthermore, individual questions were assigned to the corresponding map skills that are necessary for the formulation of the question. Younger students were found to ask significantly more questions about the map display; while older students are also interested in the geological content and the way the map was created. There was also a difference between the geological map of the Czech Republic and Prague. The students were able to obtain...
|
|
|
Komplexní geologická charakterizace prostorů PVP Bukov
Verner, K. ; Bukovská, Z. ; Souček, Kamil ; Vavro, Martin ; Staš, Lubomír ; Kaláb, Zdeněk ; Havlová, V. ; Kučera, P.
This report summarizes results of ongoing basic and applied research related to the project "Comprehensive geological characterization of underground research facility (PVP) Bukov" (PB-2014-ZL-U2301-004-BUKOV). In the wider area of the PVP Bukov a steep NW-SE trending metamorphic foliation was identified which is partly refolded into sub-horizontal direction. Faults and extensional joints with variable mineralization are mostly steep, trending mostly NW - SE or NNE - SSW. In addition, geological map at the scale of 1 : 4 500 of this area has been processed based on new field geological mapping and archival data. Moreover, a detailed petrographic and structural analysis of boreholes S-1 to S-4 (a total length of 470 meters) has been made. On the basis of U/Pb dating the age of the protolith of prevailing migmatized amphibolic gneisses was determined at 500-600 Ma as well as the subsequent regional metamorphism associated with partial melting and deformation at around 338 Ma. Results of thermodynamic modeling revealed the P-T conditions of regional metamorphism at T: 692–727 °C and P: 5 kbar.
|
guest ::
