The heads of the thick landslides are in the fill on the downhill edge of Delhi Pike. The fill contains overlapping low scarps and tension cracks (pi. 1) extending to the break in slope at the shoulder of the road. These cracks, which indicate stretching or extension of the landslide material, are confined to the fill area. All indications of landsliding farther downslope are of shortening or compression. The compressional features are difficult to recognize in natural slopes but are well expressed where they intersect a wall, road, or walkway. Figure 3 consists of two photographs of toes of deepseated landslides; locations are shown on the map of the Delhi Pike landslide complex (pi. 1).