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Eberswalde crater is located to the north of the Holden crater and is characterized by the presence of well-developed delta. The delta in Eberswalde indicates the presence of sustain water flows that carried suspended fine-grained materials into the crater from outside, from a broad depression westward of Eberswalde, the western depression, into the sink of the crater. To study the modes and timescale of the formation of the delta, we investigated the morphological characteristics of the western depression in detail. Our study was based on the topographic data (MOLA gridded topography, 1/128 degree resolution) and the mosaics of the CTX images (6 m/px resolution).