Earthwatcher's photos with the keyword: erratic

Alternating sandstones and softer siltstones/mudstones in the Bay of Stoer Formation (1200 Ma) have eroded differentially to form a series of narrow inlets at Sgèir na Tràghad, near Clachtoll. A small erratic boulder of Lewisian Gneiss rests in the foreground. The Coigach peninsula is visible on the skyline.

Alternating sandstones and softer siltstones/mudstones in the Bay of Stoer Formation (1200 Ma) have eroded differentially to form a series of narrow inlets at Sgèir na Tràghad, near Clachtoll. A small erratic boulder of Lewisian Gneiss rests in the foreground. The Coigach peninsula is visible on the skyline. A panoramic view consisting of three portrait-style photos stitched together.

Alternating sandstones and softer siltstones/mudstones in the Bay of Stoer Formation (1200 Ma) have eroded differentially to form a series of narrow inlets at Sgèir na Tràghad, near Clachtoll. An erratic boulder of Lewisian Gneiss is visible to the upper left. The Coigach peninsula is visible on the skyline.

Alternating sandstones and softer siltstones/mudstones in the Bay of Stoer Formation (1200 Ma) have eroded differentially to form a series of narrow inlets at Sgèir na Tràghad, near Clachtoll. An erratic boulder of Lewisian Gneiss is perched on the outcrop of one of the sandstones.

Alternating sandstones and softer siltstones/mudstones in the Bay of Stoer Formation (1200 Ma) have eroded differentially to form a series of narrow inlets at Sgèir na Tràghad, near Clachtoll. An erratic boulder of Lewisian Gneiss is perched on the outcrop of one of the sandstones.

One of the many erratics of Lewisian Gneiss scattered all over the Stoer peninsula, left by the retreating ice sheets of the last glaciation. This one is perched on top of westerly dipping sandstones of the Stoer Group (late Precambrian, 1.2 billion years old).

There are many erratics of Lewisian Gneiss scattered all over the Stoer peninsula, left by the retreating ice sheets of the last glaciation. There are several visible in this photo - some identified by the notes - perched on top of westerly dipping sandstones of the Stoer Group (late Precambrian, 1.2 billion years old).

One of the many erratics of Lewisian Gneiss scattered all over the Stoer peninsula, left by the retreating ice sheets of the last glaciation. This one is perched on top of westerly dipping sandstones of the Stoer Group (late Precambrian, 1.2 billion years old).

One of the many erratics of Lewisian Gneiss scattered all over the Stoer peninsula, left by the retreating ice sheets of the last glaciation. This one is perched on top of westerly dipping sandstones of the Stoer Group (late Precambrian, 1.2 billion years old).