A geodesic in a graph G is a shortest path between two vertices of G. For a specific function e(n) of n, we define an almost geodesic cycle C in G to be a cycle in which for every two vertices u and v in C, the distance d G (u, v) is at least d C (u, v)-e(n). Let (n) be any function tending to infin
Geodesics in Transitive Graphs
โ Scribed by C.Paul Bonnington; Wilfried Imrich; Norbert Seifter
- Publisher
- Elsevier Science
- Year
- 1996
- Tongue
- English
- Weight
- 541 KB
- Volume
- 67
- Category
- Article
- ISSN
- 0095-8956
No coin nor oath required. For personal study only.
โฆ Synopsis
Let P be a double ray in an infinite graph X, and let d and d P denote the distance functions in X and in P respectively. One calls P a geodesic if d(x, y)=d P (x, y), for all vertices x and y in P. We give situations when every edge of a graph belongs to a geodesic or a half-geodesic. Furthermore, we show the existence of geodesics in infinite locally-finite transitive graphs with polynomial growth which are left invariant (set-wise) under ``translating'' automorphisms. As the main result, we show that an infinite, locally-finite, transitive, 1-ended graph with polynomial growth is planar if and only if the complement of every geodesic has exactly two infinite components.
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