THE BLUE MOUNTAINS RISE to a broad plateau not far west of Sydney, Australia. In the heart of the mountains lies the Grose Valley, bounded by sheer 300-metre-high cliffs.
This dramatic landscape was sculpted by forces of erosion acting on the underlying geology; that is, characteristics of each rock type helped determine the topography.
This natural-colour satellite image was acquired by the Enhanced Thematic Mapper Plus (ETM+) instrument on the Landsat 7 satellite.
Deep green forests, dominated by eucalyptus trees, cover the landscape. The light grey buildings of Blackheath lie just to the west of the valley (lower left), and the light green orchards and pastures surrounding Berambing are visible to the northeast (upper right).
Two main types of rocks make up the Grose Valley and the immediate surroundings: a young, thin layer of volcanic rock, and a thick sequence of sedimentary rocks, laid down by wind and water several hundred million years ago. Several distinct types of shale, sandstone, and siltstone appear in the sedimentary sequence, which comprises the bedrock in most of this image.
The topmost layer is comprised of basalt erupted 15 to 18 million years ago from an unknown source. Most of this basalt has eroded away, but some can still be found at high points like Mount Tomah. Soils in these areas support a unique ecosystem called Tableland Basalt Forest, which appears bright green in this image.
Directly beneath the basalt are Wianamatta Group shales, followed by the Hawkesbury Sandstone—which forms the cliffs along the Sydney coast, 100 kilometres to the east. These two rock layers are softer than the basalt above and the sandstone below, so they have mostly eroded away except where protected by a cap of basalt.
Beneath the Wianamatta Group and Hawkesbury Sandstone are layers of very hard sandstone called the Narrabeen Group. These 240 million-year-old sandstones resist erosion and form the sheer cliffs that surround Grose Valley.
Softer shales and sandstones, the “Coal Measures,” underlie the Narrabeen sandstones and make up the slopes visible beneath the cliffs. Coal and oil shales in these formations have been mined extensively.
At the base of the valley is Berry Siltstone, originally deposited on an ocean floor over 260 million years ago. The Grose River flows atop this siltstone, carrying freshly eroded sand grains eastwards to the ocean.
See the full-size image of the Blue Mountains from space.
Text adapted from information issued by Robert Simmon. NASA Earth Observatory image by Jesse Allen and Robert Simmon, with Landsat data from the USGS Global Visualization Viewer. Landsat graphic courtesy NASA.
Get SpaceInfo.com.au daily updates by RSS or email! Click the RSS Feed link at the top right-hand corner of this page, and then save the RSS Feed page to your bookmarks. Or, enter your email address (privacy assured) and we’ll send you daily updates. Or follow us on Twitter, @spaceinfo_oz
Like this story? Please share or recommend it…