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  2. Five themes of geography - Wikipedia

    en.wikipedia.org/wiki/Five_themes_of_geography

    Most American geography and social studies classrooms have adopted the five themes in teaching practices, [3] as they provide "an alternative to the detrimental, but unfortunately persistent, habit of teaching geography through rote memorization". [1] They are pedagogical themes that guide how geographic content should be taught in schools. [4]

  3. Group cohesiveness - Wikipedia

    en.wikipedia.org/wiki/Group_cohesiveness

    Group cohesiveness, also called group cohesion, social harmony or social cohesion, is the degree or strength of bonds linking members of a social group to one another and to the group as a whole. [1] Although cohesion is a multi-faceted process, it can be broken down into four main components: social relations , task relations, perceived unity ...

  4. Cohesion (linguistics) - Wikipedia

    en.wikipedia.org/wiki/Cohesion_(linguistics)

    Cohesion is the grammatical and lexical linking within a text or sentence that holds a text together and gives it meaning. It is related to the broader concept of coherence. There are two main types of cohesion: grammatical cohesion: based on structural content; lexical cohesion: based on lexical content and background knowledge.

  5. Thematic learning - Wikipedia

    en.wikipedia.org/wiki/Thematic_Learning

    Themes allowing past to present connections and highlight persistent issued faced by society such as war, poverty, pollution, disease, or natural disasters are especially effective. [4] Doing the research: Effective interdisciplinary thematic instruction requires extensive knowledge and research by the teacher. Without a broad knowledge base on ...

  6. Deposition (geology) - Wikipedia

    en.wikipedia.org/wiki/Deposition_(geology)

    Deposition of non-cohesive sediments [ edit ] Large-grain sediments transported by either bedload or suspended load will come to rest when there is insufficient bed shear stress and fluid turbulence to keep the sediment moving; [ 4 ] with the suspended load this can be some distance as the particles need to fall through the water column.

  7. River bank failure - Wikipedia

    en.wikipedia.org/wiki/River_bank_failure

    A river bank will respond to erosional activity based on the characteristics of the bank material. The most common type of bank is a stratified or interstratified bank, which consists of cohesionless layers interbedded with cohesive layers. [5] If the cohesive soil is at the toe of the bank, it will control the retreat rate of the overlying layer.

  8. Cohesion (geology) - Wikipedia

    en.wikipedia.org/wiki/Cohesion_(geology)

    Cohesion is the component of shear strength of a rock or soil that is independent of interparticle friction. In soils, true cohesion is caused by following: Electrostatic forces in stiff overconsolidated clays (which may be lost through weathering) Cementing by Fe 2 O 3, Ca CO 3, Na Cl, etc. There can also be apparent cohesion. This is caused by:

  9. Portal:Geography/Intro/8 - Wikipedia

    en.wikipedia.org/wiki/Portal:Geography/Intro/8

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Donate; Help; Learn to edit; Community portal; Recent changes; Upload file

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