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Near the carpark of Mt Williams’ peak, Grampians National Park.

The resulting rocks are in the form of alternating beds of highly resistant quartzose sandstone and layers of less resistant siltstone and mudstone. Subsequent folding of these rocks produced the ranges with sloping sandstone and shale strata, as well as grey granite intrusions. Later erosion has removed much of the shale leaving the more resistant sandstone in asymmetrical ridges, often with steep east-facing escarpments, and with sloping western sides. This formation has been called a cuesta. Fyans Valley, between the Serra Range and the Mt William Range, can be viewed from Boroka Lookout.From: http://austhrutime.com/grampian_ranges.htm 

Near the carpark of Mt Williams’ peak, Grampians National Park.

The resulting rocks are in the form of alternating beds of highly resistant quartzose sandstone and layers of less resistant siltstone and mudstone. Subsequent folding of these rocks produced the ranges with sloping sandstone and shale strata, as well as grey granite intrusions. Later erosion has removed much of the shale leaving the more resistant sandstone in asymmetrical ridges, often with steep east-facing escarpments, and with sloping western sides. This formation has been called a cuesta. Fyans Valley, between the Serra Range and the Mt William Range, can be viewed from Boroka Lookout.

From: http://austhrutime.com/grampian_ranges.htm 

View of Halls Gap and Lake Bellfield yonder from the Boroka Lookout.

View of Halls Gap and Lake Bellfield yonder from the Boroka Lookout.

A view from Boroka Lookout, Grampians National Park.

A view from Boroka Lookout, Grampians National Park.

This Scarlet Robin likes checking himself out in reflective objects such as this car side-mirror.

This Scarlet Robin likes checking himself out in reflective objects such as this car side-mirror.

Moss on rocks at high altitude!

Moss on rocks at high altitude!

View of Lake Wartook from on a point on the trail to The Balconies.

View of Lake Wartook from on a point on the trail to The Balconies.

View of Moora Moora Reservoir from The Balconies, Grampians National Park.

View of Moora Moora Reservoir from The Balconies, Grampians National Park.

The Balconies, Grampians National Park. Looks like a spanner. 

The Balconies, Grampians National Park. Looks like a spanner.

 

Crimson Rosellas carry on eating despite being watched by an annoying human.

Crimson Rosellas carry on eating despite being watched by an annoying human.

I did not feed the Crimson Rosellas; the seeds were already there when I spotted them on the table!People should try not to feed wild birds. But if they do, at least provide food suited to the species. :)

I did not feed the Crimson Rosellas; the seeds were already there when I spotted them on the table!

People should try not to feed wild birds. But if they do, at least provide food suited to the species. :)

Model: Kennie

Model: Kennie

A happy groom!

A happy groom!

Model: Katrina

Model: Katrina

Model: Katrina

Model: Katrina

Near the carpark of Mt Williams’ peak, Grampians National Park.

The resulting rocks are in the form of alternating beds of highly resistant quartzose sandstone and layers of less resistant siltstone and mudstone. Subsequent folding of these rocks produced the ranges with sloping sandstone and shale strata, as well as grey granite intrusions. Later erosion has removed much of the shale leaving the more resistant sandstone in asymmetrical ridges, often with steep east-facing escarpments, and with sloping western sides. This formation has been called a cuesta. Fyans Valley, between the Serra Range and the Mt William Range, can be viewed from Boroka Lookout.From: http://austhrutime.com/grampian_ranges.htm 

Near the carpark of Mt Williams’ peak, Grampians National Park.

The resulting rocks are in the form of alternating beds of highly resistant quartzose sandstone and layers of less resistant siltstone and mudstone. Subsequent folding of these rocks produced the ranges with sloping sandstone and shale strata, as well as grey granite intrusions. Later erosion has removed much of the shale leaving the more resistant sandstone in asymmetrical ridges, often with steep east-facing escarpments, and with sloping western sides. This formation has been called a cuesta. Fyans Valley, between the Serra Range and the Mt William Range, can be viewed from Boroka Lookout.

From: http://austhrutime.com/grampian_ranges.htm 

View of Halls Gap and Lake Bellfield yonder from the Boroka Lookout.

View of Halls Gap and Lake Bellfield yonder from the Boroka Lookout.

A view from Boroka Lookout, Grampians National Park.

A view from Boroka Lookout, Grampians National Park.

This Scarlet Robin likes checking himself out in reflective objects such as this car side-mirror.

This Scarlet Robin likes checking himself out in reflective objects such as this car side-mirror.

Moss on rocks at high altitude!

Moss on rocks at high altitude!

View of Lake Wartook from on a point on the trail to The Balconies.

View of Lake Wartook from on a point on the trail to The Balconies.

View of Moora Moora Reservoir from The Balconies, Grampians National Park.

View of Moora Moora Reservoir from The Balconies, Grampians National Park.

The Balconies, Grampians National Park. Looks like a spanner. 

The Balconies, Grampians National Park. Looks like a spanner.

 

Crimson Rosellas carry on eating despite being watched by an annoying human.

Crimson Rosellas carry on eating despite being watched by an annoying human.

Rarr, my feet is itchy!

Rarr, my feet is itchy!

I did not feed the Crimson Rosellas; the seeds were already there when I spotted them on the table!People should try not to feed wild birds. But if they do, at least provide food suited to the species. :)

I did not feed the Crimson Rosellas; the seeds were already there when I spotted them on the table!

People should try not to feed wild birds. But if they do, at least provide food suited to the species. :)

About:

The toes of my foe.