National Repository of Grey Literature 106 records found  beginprevious104 - 106  jump to record: Search took 0.00 seconds. 
The teaching of region-general science on the Klatovsko example
NOVOTNÁ, Anežka
The aim of this diploma thesis is The teaching of region-general science on the Klatovsko example. In the first part of the work is the theoretical introduction composed from special literature which describes Klatovsko in many views. The region is characterized, defined and divided to the sub regions; either physical-geographical and socio-economical data as well as environment-conservation are reviewed in the theoretical part of this thesis. The work is not focused only on range of general science but also logical attaches it with information from regional geography. This data together gives allover review on the resolved region. The necessary part of this diploma these is own resolving which is based on seeking for knowledge about the region in 4th and 5th classes of elementary schools. The little spread method of mental mapping was used for research and the method was extended with questionary investigation. The results of own resolving are discussed and interpreted by suitable graphs. The teaching-utilities for either region-general science and geography were created on base of obtained results. The learning texts are prepared for direct-teaching of pupils and connected working sheets for reviewing their knowledge and quality-control of teaching were attached. As an alternative learning-method the funny projects are provided with this work. These projects are useful for teaching of Klatovy region.
Enhancement of knowledge about geomorphological development of the Obora site NW from Brno with using geoelectric sounding.
Peterková, L. ; Kirchner, Karel ; Hubatka, F. ; Nehyba, S.
Contributions deals with geomorphological a sedimentological research in the Obora site (flat depression in the middle part of Svratka river valley) with using georadar and geoelectric sounding. Aim of investigation – recognition of the character Lower Badenian sediments with aspects of position and form of bed rock in the deep valley. Application of geophysical methods enables to distinguish three sedimentational phases of Lower Badenian sediments.

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