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Vestfold is the old name of the region which was revived in modern times. Fold was the old name of the Oslofjord, and the meaning of the name Vestfold is the region west of the Fold (see also Østfold). Before 1919, the county was called Jarlsberg og Larvik Amt.
The Alx4 region, the medial region, and the Hox8 expressing area meet at a proximal area where the AER develops. The ZPA forms where the Hox8 region joins the AER. These regions are dependent on signaling in order for the appropriate induction events to occur. The AER expresses FGF8 which induces Shh expression in the posterior mesoderm.
The size and the borders of each region are defined by geologically significant boundaries and by the occurrence of geologic processes. [1] Examples of geologically significant boundaries are the interfingering facies change in sedimentary deposits when discussing a sedimentary basin system, or the leading or boundary thrust of an orogen. [2]
Advancements in molecular biology and theory of evolution within zoological research has unraveled questions concerning speciation events and has expanded phylogenic relationships amongst taxa. [3] Integration of phylogenetics with GIS provides a means for communicating evolutionary origins through cartographic design.
The region of Vestfold and Telemark consists of the two former counties of Telemark and Vestfold, whose administrative histories are separate. Telemark County was established in 1919 as a continuation of the former Bratsberg amt, which had been a len and amt since the union with Denmark.
Beyond "vernacular geography," a "vernacular region" is a distinctive area where the inhabitants collectively consider themselves interconnected by a shared history, mutual interests, and a common identity. Such regions are "intellectual inventions" and a form of shorthand to identify things, people, and places.
The apical ectodermal ridge (AER) is a structure that forms from the ectodermal cells at the distal end of each limb bud and acts as a major signaling center to ensure proper development of a limb.
The Vestfold Hills are rounded, rocky, coastal hills, 512 square kilometres (198 sq mi) in extent, [1] [2] on the north side of Sorsdal Glacier on the Ingrid Christensen Coast of Princess Elizabeth Land, Antarctica. The hills are subdivided by three west-trending peninsulas bounded by narrow fjords.