near the Elvina Track on the Park's Lambert Peninsular|thumb|left Ku-ring-gai Chase is part of the
Hornsby Plateau, a massive block of sandstone tilting upwards to the north. The park comprises a plateau with an elevation of generally 150–200 m above sea level. Between 250 and 200 million years ago, sand silt and mud was deposited by rivers across flood plains. Other rock types in the park are less common. Soils derived from the
Narrabeen group of shales are around the eastern shore of the Lambert Peninsula, particularly around
Elvina Bay and
Lovett Bay. These richer soils provide for a vegetation type different from that of the sandy ridge top soils, providing for forests of spotted gums (
Corymbia maculata) with forest oaks as a secondary layer. Eroded remnants of volcanic dykes occur including at Resolution Picnic Area at
West Head and Campbells Crater near
Cowan, which provide for forests of Sydney blue gum (
Eucalyptus saligna). More recent volcanic activity has forced small intrusions of igneous rock into the sandstone. A band of
dolerite runs across the
West Head peninsula near White Horse Beach, providing fertile soils for a distinct group of plants. The Smith's Creek area has intrusions of
breccia. The plateau is divided into separate sections by the steep valleys of
Cowan Creek,
Coal and Candle Creek, and
Smiths Creek. These "flooded" or "drowned" valleys, knowns as
rias, were eroded into the sandstone much deeper than the current sea level during the glacial phases of the
Pleistocene ice age. When the ice caps melted about 10,000 years ago, the sea levels rose and flooded the valleys of the park, and separated
Lion and
Scotland islands from the mainland. The tributaries of Pittwater and Cowan Creek became bays and inlets along and extended shoreline. The dominant rock type is
Hawkesbury Sandstone which determines the topography and the vegetation in the sandy soils. Sandstone cliffs, rocky and outcrops, and worn caves are common throughout the park. Indigenous people engraved the flat sandstone outcrops.
Tessellated pavements are found in the park whereby regular chequered patterns in the stone form along fault lines and lines of weakness. The park's highest point is 246 m at Willunga Trig near West Head Road which runs along the ridge of the Lambert Peninsula. ==History==