Bending of a surface conserves parallelism between any two initially parallel geodesic lines.
Can some examples be given from hyperbolic geometry ? How are bent surface hyperbolic geodesic parallel lines understood in the three models?
Bending of a surface conserves parallelism between any two initially parallel geodesic lines.
Can some examples be given from hyperbolic geometry ? How are bent surface hyperbolic geodesic parallel lines understood in the three models?
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