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This report is focused to describe the main alpine structures located in the northern edge of the Spanish Central System and the linking zone with the Tertiary Duero basin. A review of the main characteristics of the alpine tectonic phases is given. From these data, differences between the Gredos zone, dominated by N-S and E-W faults, and the Guadarrama zone, in which N 70&#194;&#176; E reverse faults with N 140&#194;&#176; E and N 10&#194;&#176; E strike-slip faults are present, can be observed. The pattern of drainage of this area shows three main orientations, coincident with the alpine faults activated during the Guadarrama tectonic phase, which reveals the relationship between the present drainage pattern and the Alpine orogeny.  En este trabajo se describen las principales estructuras alpinas del borde norte del Sistema Central y su enlace con la cuenca del Duero, as&#237; como las caracter&#237;sticas de las principales fases tect&#243;nicas alpinas que han dado lugar a la actual estructura. Se pone de manifiesto las diferencias entre la zona de Gredos, dominada por fallas N-S y E-O principalmente, y la zona de Guadarrama en la que las fallas inversas son N 70&#194;&#176; E acompa&#241;adas de desgarres N 140&#194;&#176; E y N 10&#194;&#176; E. El an&#225;lisis de las direcciones de los r&#237;os en este &#225;rea permite definir tres zonas en funci&#243;n de su orientaci&#243;n, que coinciden con las definidas para las fallas alpinas, lo que refleja la relaci&#243;n entre la red de drenaje y la fase alpina Guadarrama principalmente

La tectónica alpina en el borde norte del Sistema Central español y su enlace con la cuenca del Duero