On the mild and wild mechanical roughness of the lithosphere

摘要: The spatio-temporal mechanical fractality of the lithosphere can be represented by means Levy-statistics and fractional calculus. This novel concept is outlined with geometrical energetic arguments. originates from pore system appears in displacements, stresses seismicity. It shown that roughness may neglected for stable range, but not critical phenomena at verge convexity. outline leads rough coastlines via sand samples to tectonic chain reactions. Equations theorems are physically interpreted without algebra proofs.Keywords: fractality, lithosphere, roughnessLa fractalidad mecanica espacio-temporal de la litosfera puede ser representada por medio estadistica Levy y calculo fraccional. Este nuevo concepto es planteado con argumentos geometricos energeticos. La se origina del sistema poroso aparece en desplazamientos, tensiones sismicidad. Se muestra que rugosidad podria no considerada el rango estable, pero esto posible fenomenos criticos al borde convexidad energetica. planteamiento cubre bordes costeros rugosos, muestras arena reacciones tectonicas cadena. Ecuaciones teoremas son interpretados fisicamente sin necesidad ni pruebas.Palabras clave: fractalidad, litosfera,