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For today's get away, we will visit the Tasman Peninsula about 90 minutes drive from Hobart, the capital of Tasmania. The Tasman Peninsula is home to stunning natural formations such as the Tesselated Pavement, Devil’s Kitchen, Tasman Arch, Tasman Blow Hole and the Port Arthur Historic Site.
This photo is from the Tessellated Pavement at Lufra, Eaglehawk Neck on the Tasman Peninsula. This tessellated pavement consists of a marine platform on the shore of Pirates Bay where there are two types of formations: a pan formation and a loaf formation. Here we see the loaf formation.
Eaglehawk Neck is a narrow isthmus that connects the Tasman Peninsula with the Forestier Peninsula, and hence to mainland Tasmania, Australia. A township settlement in the same region is also called Eaglehawk Neck. Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. The area features rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. A short walk further via Lufra Cove leads to Clyde Island, accessible for crossings at low tide, which sits at the northern entry to Pirates Bay. The island hosts two grave sites, and a rumbling blow hole cleaves the island. Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes. 29052
Eaglehawk Neck is a narrow isthmus that connects the Tasman Peninsula with the Forestier Peninsula, and hence to mainland Tasmania, Australia. A township settlement in the same region is also called Eaglehawk Neck. Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. The area features rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. A short walk further via Lufra Cove leads to Clyde Island, accessible for crossings at low tide, which sits at the northern entry to Pirates Bay. The island hosts two grave sites, and a rumbling blow hole cleaves the island. Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes. 29013
Eaglehawk Neck is a narrow isthmus that connects the Tasman Peninsula with the Forestier Peninsula, and hence to mainland Tasmania, Australia. A township settlement in the same region is also called Eaglehawk Neck. Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. The area features rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. A short walk further via Lufra Cove leads to Clyde Island, accessible for crossings at low tide, which sits at the northern entry to Pirates Bay. The island hosts two grave sites, and a rumbling blow hole cleaves the island. Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes. 29011
Eaglehawk Neck is a narrow isthmus that connects the Tasman Peninsula with the Forestier Peninsula, and hence to mainland Tasmania, Australia. A township settlement in the same region is also called Eaglehawk Neck. Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. The area features rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. A short walk further via Lufra Cove leads to Clyde Island, accessible for crossings at low tide, which sits at the northern entry to Pirates Bay. The island hosts two grave sites, and a rumbling blow hole cleaves the island. Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes. 29034
Eaglehawk Neck is a narrow isthmus that connects the Tasman Peninsula with the Forestier Peninsula, and hence to mainland Tasmania, Australia. A township settlement in the same region is also called Eaglehawk Neck. Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. The area features rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. A short walk further via Lufra Cove leads to Clyde Island, accessible for crossings at low tide, which sits at the northern entry to Pirates Bay. The island hosts two grave sites, and a rumbling blow hole cleaves the island. Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes. 29040
This image is included in a gallery "Photo Gallery" curated by Ryan Miller.
Located about 77 km from Hobart, it is an easy drive of just over an hour. In geology and geomorphology, a tessellated pavement is a relatively flat rock surface that is subdivided into more or less regular rectangles, blocks approaching rectangles, or irregular or regular polygons by fractures, frequently systematic joints, within the rock. This type of rock pavement bears this name because it is fractured into polygonal blocks that resemble tiles of a mosaic floor, or tessellations.
The most well-known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tessellated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
The pan formation is a series of concave depressions in the rock that typically forms beyond the edge of the seashore. This part of the pavement dries out more at low tide than the portion abutting the seashore, allowing salt crystals to develop further; the surface of the "pans" therefore erodes more quickly than the joints, resulting in increasing concavity.
The loaf formation occurs on the parts of the pavement closer to the seashore, which are immersed in water for longer periods of time. These parts of the pavement do not dry out so much, reducing the level of salt crystallisation. Water, carrying abrasive sand, is typically channelled through the joints, causing them to erode faster than the rest of the pavement, leaving loaf-like structures protruding.
This backlit image here shows a fine example of the loaf-like formation. Looking beyond the horizon is Tasman Sea.
A beautiful dawn unfolded before my eyes as I left Tasman Peninsula. The best thing about this shoot, staying 5 minutes walk away at the Lufra hotel as an overnighter between hikes made this very easy to rush out to after I saw light was on!
Located about 77 km from Hobart, it is an easy drive of just over an hour. In geology and geomorphology, a tessellated pavement is a relatively flat rock surface that is subdivided into more or less regular rectangles, blocks approaching rectangles, or irregular or regular polygons by fractures, frequently systematic joints, within the rock. This type of rock pavement bears this name because it is fractured into polygonal blocks that resemble tiles of a mosaic floor, or tessellations.
The most well-known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tessellated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
The pan formation is a series of concave depressions in the rock that typically forms beyond the edge of the seashore. This part of the pavement dries out more at low tide than the portion abutting the seashore, allowing salt crystals to develop further; the surface of the "pans" therefore erodes more quickly than the joints, resulting in increasing concavity.
The loaf formation occurs on the parts of the pavement closer to the seashore, which are immersed in water for longer periods of time. These parts of the pavement do not dry out so much, reducing the level of salt crystallisation. Water, carrying abrasive sand, is typically channelled through the joints, causing them to erode faster than the rest of the pavement, leaving loaf-like structures protruding.
This backlit image here shows a fine example of the pan formation.
My daughter exploring the staircase of an art deco hotel, 'The Lufra Hotel', at a place called Eaglehawk Neck in Tasmania. By virtue of its name, the place reminded me of the song 'The Eagle and the Hawk' from my childhood, and seeing my daughter there rising into the surreal staircase just called for this title. Taken with my iPhone as I didn't have my camera with me.
Eaglehawk Neck is a narrow isthmus that connects the Tasman Peninsula with the Forestier Peninsula, and hence to mainland Tasmania, Australia. A township settlement in the same region is also called Eaglehawk Neck. Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. The area features rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. A short walk further via Lufra Cove leads to Clyde Island, accessible for crossings at low tide, which sits at the northern entry to Pirates Bay. The island hosts two grave sites, and a rumbling blow hole cleaves the island. Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes. 29023
Eaglehawk Neck is a narrow isthmus that connects the Tasman Peninsula with the Forestier Peninsula, and hence to mainland Tasmania, Australia. A township settlement in the same region is also called Eaglehawk Neck. Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. The area features rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. A short walk further via Lufra Cove leads to Clyde Island, accessible for crossings at low tide, which sits at the northern entry to Pirates Bay. The island hosts two grave sites, and a rumbling blow hole cleaves the island. Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes. 29014
Eaglehawk Neck is a narrow isthmus that connects the Tasman Peninsula with the Forestier Peninsula, and hence to mainland Tasmania, Australia. A township settlement in the same region is also called Eaglehawk Neck. Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. The area features rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. A short walk further via Lufra Cove leads to Clyde Island, accessible for crossings at low tide, which sits at the northern entry to Pirates Bay. The island hosts two grave sites, and a rumbling blow hole cleaves the island. Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes. 29032
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tessellated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
The pan formation is a series of concave depressions in the rock that typically forms beyond the edge of the seashore. This part of the pavement dries out more at low tide than the portion abutting the seashore, allowing salt crystals to develop further; the surface of the "pans" therefore erodes more quickly than the joints, resulting in increasing concavity.
The loaf formations occur on the parts of the pavement closer to the seashore, which are immersed in water for longer periods of time. These parts of the pavement do not dry out so much, reducing the level of salt crystallisation. Water, carrying abrasive sand, is typically channelled through the joints, causing them to erode faster than the rest of the pavement, leaving loaf-like structures protruding.
Source: Wikipedia
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tessellated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
The pan formation is a series of concave depressions in the rock that typically forms beyond the edge of the seashore. This part of the pavement dries out more at low tide than the portion abutting the seashore, allowing salt crystals to develop further; the surface of the "pans" therefore erodes more quickly than the joints, resulting in increasing concavity.
The loaf formations occur on the parts of the pavement closer to the seashore, which are immersed in water for longer periods of time. These parts of the pavement do not dry out so much, reducing the level of salt crystallisation. Water, carrying abrasive sand, is typically channelled through the joints, causing them to erode faster than the rest of the pavement, leaving loaf-like structures protruding.
Source: Wikipedia
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tessellated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
The pan formation is a series of concave depressions in the rock that typically forms beyond the edge of the seashore. This part of the pavement dries out more at low tide than the portion abutting the seashore, allowing salt crystals to develop further; the surface of the "pans" therefore erodes more quickly than the joints, resulting in increasing concavity.
The loaf formations occur on the parts of the pavement closer to the seashore, which are immersed in water for longer periods of time. These parts of the pavement do not dry out so much, reducing the level of salt crystallisation. Water, carrying abrasive sand, is typically channelled through the joints, causing them to erode faster than the rest of the pavement, leaving loaf-like structures protruding.
Source: Wikipedia
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tessellated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
The pan formation is a series of concave depressions in the rock that typically forms beyond the edge of the seashore. This part of the pavement dries out more at low tide than the portion abutting the seashore, allowing salt crystals to develop further; the surface of the "pans" therefore erodes more quickly than the joints, resulting in increasing concavity.
The loaf formations occur on the parts of the pavement closer to the seashore, which are immersed in water for longer periods of time. These parts of the pavement do not dry out so much, reducing the level of salt crystallisation. Water, carrying abrasive sand, is typically channelled through the joints, causing them to erode faster than the rest of the pavement, leaving loaf-like structures protruding.
Source: Wikipedia
In geology and geomorphology, a tessellated pavement is a relatively flat rock surface that is subdivided into more or less regular rectangles, blocks approaching rectangles, or irregular or regular polygons by fractures, frequently systematic joints, within the rock. This type of rock pavement bears this name because it is fractured into polygonal blocks that resemble tiles of a mosaic floor, or tessellations.
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tesselated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
#tasmania #australia #visitaustralia #tassie #tessellatedpavement #eaglehawknecktasmania #nature #landscape
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tessellated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
The pan formation is a series of concave depressions in the rock that typically forms beyond the edge of the seashore. This part of the pavement dries out more at low tide than the portion abutting the seashore, allowing salt crystals to develop further; the surface of the "pans" therefore erodes more quickly than the joints, resulting in increasing concavity.
The loaf formations occur on the parts of the pavement closer to the seashore, which are immersed in water for longer periods of time. These parts of the pavement do not dry out so much, reducing the level of salt crystallisation. Water, carrying abrasive sand, is typically channelled through the joints, causing them to erode faster than the rest of the pavement, leaving loaf-like structures protruding.
Source: Wikipedia
About Eaglehawk Neck
From Wikipedia
Eaglehawk Neck is a narrow isthmus connecting the Tasman Peninsula to mainland Tasmania. At the 2006 census, Eaglehawk Neck had a population of 269.
Locally known as the Neck, the isthmus itself is around 400 metres long and under 30 metres wide at its narrowest point. It forms a natural gateway to the peninsula that was utilised by the British in 1830s, when a line of dogs was chained to posts across the neck to warn of any convicts attempting to escape the prison at Port Arthur. The area was heavily patrolled by soldiers, and the guards' quarters still remains as a museum. Many attempts were made by prisoners to escape via the neck, including those of Martin Cash.
The area has a beautiful and rugged terrain and several unusual geological formations. These include the Tessellated Pavement, an area of flat rock that looks to be manmade but is in fact formed by erosion. Also nearby are Tasman's Arch, the Blowhole and the Devil's Kitchen, all striking natural formations.
Eaglehawk Neck offers accommodation in the Lufra Hotel, near the Tessellated Pavement, and the Backpackers on Jetty Road.
A nearby footpath leads to Martin Cash's lookout near the top of the hill at the southern end.
Eaglehawk Neck is a well-known local holiday destination. On the eastern side, a beach that stretches around Pirates' Bay is a popular surfing area. In summer the population rises as people return to their holiday homes.
Equipment > Nikon D90 >10mm >25secs >ISO 100 >f11 >10 Stop filter >Lee Soft Grad 0.9
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tessellated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
The pan formation is a series of concave depressions in the rock that typically forms beyond the edge of the seashore. This part of the pavement dries out more at low tide than the portion abutting the seashore, allowing salt crystals to develop further; the surface of the "pans" therefore erodes more quickly than the joints, resulting in increasing concavity.
The loaf formations occur on the parts of the pavement closer to the seashore, which are immersed in water for longer periods of time. These parts of the pavement do not dry out so much, reducing the level of salt crystallisation. Water, carrying abrasive sand, is typically channelled through the joints, causing them to erode faster than the rest of the pavement, leaving loaf-like structures protruding.
Source: Wikipedia
From Wikipedia,
A tessellated pavement at Eaglehawk Neck, Australia, where a rock surface has been divided by fractures, producing a set of rectangular blocks
In geology and geomorphology, a tessellated pavement is a relatively flat rock surface that is subdivided into more or less regular rectangles, blocks approaching rectangles, or irregular or regular polygons by fractures, frequently systematic joints, within the rock. This type of rock pavement bears this name because it is fractured into polygonal blocks that resemble tiles of a mosaic floor, or tessellations.
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tesselated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
In geology and geomorphology, a tessellated pavement is a relatively flat rock surface that is subdivided into more or less regular rectangles, blocks approaching rectangles, or irregular or regular polygons by fractures, frequently systematic joints, within the rock. This type of rock pavement bears this name because it is fractured into polygonal blocks that resemble tiles of a mosaic floor, or tessellations.
The most well known example of a tessellated pavement is the Tessellated Pavement that is found at Lufra, Eaglehawk Neck on the Tasman Peninsula of Tasmania. This tesselated pavement consists of a marine platform on the shore of Pirates Bay, Tasmania. This example consists of two types of formations: a pan formation and a loaf formation.
#tasmania #australia #visitaustralia #tassie #tessellatedpavement #eaglehawknecktasmania #nature #landscape
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Sono stato "taggato" contemporaneamente da Plastic Sergio e da Lufra
... devo scrivere 16 cose che probabilmente non sapete di me.
1 - odio guidare la macchina
2 - so suonare il marranzano
3- ho visto tutti proprio tutti gli episodi di star trek
4- mi faccio io le sigarette che fumo
5- mi hanno battezzato a trent'anni
6- mi piace il lego
7- so giocare a scacchi
8- adoro la cuccìa
9 - ho più di cento cravatte ma non le indosso mai
10 - non ho più la cistifellea
11 - mia madre non mi capisce
12 - non ho più l'età per fare certe cose, ma le faccio lo stesso
13 - mio nonno era medico, ma aveva per passione una fabbrica di carrettini siciliani
14 - l'altro mio nonno era direttore del totocalcio. giocava sempre e non vinceva mai
15 - penso che potrei vivere soltanto a palermo
16 - da piccolo andavo sempre a mare a pescare i ricci. ora si sono estinti
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i ve been "tagged" by Plastic Sergio and Lufra
so there you go 16 things you probably dont know about me:
1 - i hate driving cars
2 - i can play the marranzano (sicilian musical instrument)
3 - i've seen the whole star trek series
4 - my cigarettes, i roll them up myself
5 - i was baptised at the age of 30
6 - i love lego
7 - can play chess
8 - love cuccìa (typical sicilian dish)
9 - i own more than 100 ties (but never wear a single one)
10 - dont have my gallbladder anymore
11 - my mother doesnt understand me
12 - i m too old for doing certain things, but i do them anyway
13 - my grandfather was a doctor but as a hobby he had a factory of carretti siciliani
14 - other grandfather was the director of the national lottery. he always used to play but never won a thing
15 - i think i could only live in palermo
16 - when i was a kid i used to go fishing "ricci di mare" (seafood), right before their extinction