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A picture of some Ammonite fossils I found in the wall of a neighbour's villa.

 

I found these one week after finding Ammonite fossils in a pavement which used a similar rock. This desert rock apparently has many Ammonite fossils, and these specimens are quite large, being about 35-40 cm wide.

 

This kind of rock is quarried in Jordan (either in the north or near the Iraqi border).

 

Ammonites are extinct marine animals that lived about 65.5 to 425 million years ago.

 

Photo taken on 05/01/2009 in Amman, Jordan.

 

Camera: Fujifilm FinePix F100fd.

postsecret.com

 

These postcards are collected from the postsecret.com blog. Though none of these are mine, many of them could be.

The Eleven Drawings (Day 3)

 

Finally… here’s my third illustration inspired by extinct and endangered animals and plants in Malaysia.

 

Black Shrew (white toothed mouse-like, Mount Kinabalu, Sabah), Tapir, Double-banded Argus (a mysterious peacock), Sarawak Shorea (extinct 1996) and Woolly-stalked Begonia (extinct 1997, Penang).

 

yinyeetai.tumblr.com

Extinct monsters and creatures of other days : a popular account of some of the larger forms of ancient animal life / by Rev. H. N. Hutchinson. With illustrations by J. Smit, Alice B. Woodward, J. Green, Charles Knight, and others.

 

London : Chapman & Hall, 1910.

 

biodiversitylibrary.org/bibliography/40362

Canon FD 50/1.4

Delta del Ebro.

Ese vicio de fotografiar fotógrafos.

Kingdom=Animalia

Phylum=Cnidaria

Class=Anthozoa

Order=Tabulata

Family=Favositidae

Genus=Favosites?

common name=extinct honeycomb coral

The horse family has lived in North America for about 50 million years. Beginning with an ancestor only two feet tall, horses have increased in size and diversity throughout their long history. They migrated to Europe, Asia and Africa before becoming extinct in the New World at the end of the Pleistocene. The wild mustangs found in the west today are descendants of modern horses brought to the New World by the early Spanish conquistadors.

Shooting for the french brand Extinct Eyes

 

Photographer: Florent Joannès

Model: Alice Valaka

Beanie & shirt: Mélodie Vesco

  

2015

Superdomain: Neomura

Domain: Eukaryota

(unranked): Unikonta

(unranked): Obazoa

(unranked): Opisthokonta

(unranked) Holozoa

(unranked) Filozoa

Kingdom: Animalia

Subkingdom: Eumetazoa

Clade: ParaHoxozoa

Clade: Bilateria

Clade: Nephrozoa

Superphylum: Deuterostomia

Phylum: Chordata

Clade: Olfactores

Subphylum: Vertebrata

Infraphylum: Gnathostomata

Clade: Eugnathostomata

Class: Chondrichthyes

Subclass: Holocephali

Superorder: Holocephalimorpha

Order: Chimaeriformes

Suborder: Squalorajoidei

Family: †Squalorajidae

Genus: †Squaloraja

Species: †S. polyspondyla

Superdomain: Neomura

Domain: Eukaryota

(unranked): Unikonta

(unranked): Obazoa

(unranked): Opisthokonta

(unranked) Holozoa

(unranked) Filozoa

Kingdom: Animalia

Subkingdom: Eumetazoa

Clade: ParaHoxozoa

Clade: Bilateria

Clade: Nephrozoa

Superphylum: Deuterostomia

Phylum: Chordata

Clade: Olfactores

Subphylum: Vertebrata

Infraphylum: Gnathostomata

Clade: Eugnathostomata

Class: Chondrichthyes

Subclass: Elasmobranchii

Infraclass: Euselachii

Superorder: Squalomorphii

Order: Hexanchiformes

Family: Hexanchidae

Genus: Hexanchus

Species: H. microdon†

Extinct monsters : a popular account of some of the larger forms of ancient animal life / by Rev. H. N. Hutchinson ... with illustrations by J. Smit and others.

 

London : Chapman & Hall, 1896.

 

www.biodiversitylibrary.org/bibliography/14948

14/03/2009 Glyptodon, at the Natural History Museum, London. Wikipedia says they were the size of a VW Beetle - perhaps this was a baby. Taken during a visit to see the Wildlife Photographer of the Year show, which made me feel rather the way this chap seems to - depressed by my own inadequacy.

The quotation comes from Emma Teitel, writing in Macleans Magazine.

 

The modified image is from an original photo of my own.

 

Seen opearting on the 603 service to London is Badgerline 2505 D505GHY a Volvo B10M / Vanhool Alizee C52FT note the inswinging door instead of the usual Plug Type fitted to Vanhools

Superdomain: Neomura

Domain: Eukaryota

(unranked): Unikonta

(unranked): Obazoa

(unranked): Opisthokonta

(unranked) Holozoa

(unranked) Filozoa

Kingdom: Animalia

Subkingdom: Eumetazoa

Clade: ParaHoxozoa

Clade: Bilateria

Clade: Nephrozoa

Superphylum: Deuterostomia

Phylum: Chordata

Clade: Olfactores

Subphylum: Vertebrata

Infraphylum: Gnathostomata

Clade: Eugnathostomata

Class: Chondrichthyes

Subclass: Elasmobranchii

Infraclass: Euselachii

Superorder: Galeomorphii

Order: Lamniformes

Family: †Otodontidae

Genus: †Otodus

Species: O. auriculatus

Skeleton of Sarcosuchus imperator at Galerie de Paleontologie, Paris.

 

Sarcosuchus imperator Broin & Taquet, 1966

Pholidosauridae

Clade: Crocodylomorpha

Long dormant volcano. Budj Bim is the source of the Tyrendarra lava flow which extends over 50km to the southwest. It is central to the history of the Gunditjmara people.

 

Mount Eccles National Park is Victoria’s first co-managed national park. The park is managed by Gunditjmara Traditional Owners and Parks Victoria.

 

The park’s tranquil crater lake and pleasant bushland surrounds make it a pleasant place for picnicking, camping and bushwalking. Nature trails follow the old crater rim.

He lives over the kitchen table. I did not make him, he is boughten.

The skeletal remains of a Pliosaur at the Royal Ontario Museum. Pliosauroidea is an extinct clade of marine reptiles. Pliosauroids, also commonly known as pliosaurs, are known from the Jurassic and Cretaceous Periods.

Superdomain: Neomura

Domain: Eukaryota

(unranked): Unikonta

(unranked): Obazoa

(unranked): Opisthokonta

(unranked) Holozoa

(unranked) Filozoa

Kingdom: Animalia

Subkingdom: Eumetazoa

(unranked): Bilateria

Superphylum: Deuterostomia

Phylum: Chordata

Subphylum: Vertebrata

Infraphylum: Gnathostomata

Superclass: Osteichthyes

Clade: Sarcopterygii

Class: Dipnoi

Order: Ceratodontiformes

Family: †Ceratodontidae

Genus: †Ceratodus

Species: †C. hieroglyphus

takeshiyamada.weebly.com/

 

The Sea Rabbit (Monafluffchus americanus) of Coney Island, Brooklyn, New York – This unique sea-dwelling rabbit, which is actually a close relative of the sea lion, was officially discovered and investigated by Henry Hudson when he first visited this land to colonize the area by order of the Dutch government. It was named New Amsterdam -- today’s New York City. This island was named after he saw the beach covered with strange swimming wild rabbits. The word “Coney Island” means “wild rabbit island” in Dutch (originally Conyne Eylandt, or Konijneneiland in modern Dutch spelling). Sea rabbits were also referred mermaid rabbit, merrabbit, rabbit fish or seal rabbit in the natural history documents in the 17th century. The current conservation status, or risk of extinction, of the sea rabbit is Extinct in the Wild.

 

This website features two species of sea rabbits, which have been taken care of by Dr. Takeshi Yamada (山田武司) at the Coney Island Sea Rabbit Repopulation Center, which is a part of the Marine biology department of the Coney Island University in Brooklyn, New York. They are – Coney Island Sea Rabbit (Monafluffchus americanus) called “Seara” and Coney Island Tiger-striped Sea Rabbit (Monafluffchus konjinicus) called “Stripes”.

 

The photographs and videos featured in this website chronicle adventures of the Coney Island sea rabbits and the world as seen by them. This article also documented efforts of Dr. Takeshi Yamada for bringing back the nearly extinct sea rabbits to Coney Island in the City of New York and beyond. Dr. Yamada produced a series of public lectures, workshops, original public live interactive fine art performances and fine art exhibitions about sea rabbits at a variety of occasions and institutions in the City of New York and beyond. Dr. Yamada is an internationally active educator, book author, wildlife conservationist and high profile artist, who lives and works in Brooklyn, New York.

 

-----------------------------------------------------------------------------------------------

 

Sea Rabbit

 

Other Common Names: Coney Island Sea Rabbit, Beach Rabbit, Seal Rabbit, mer-rabbit, merrabbit, Atlantic Sea Rabbit.

 

Latin Name: Monafluffchus americanus

 

Origin: Atlantic coast of the United States

 

Description of the specimen: In the early 17th century’s European fur craze drove the fleet of Dutch ships to the eastern costal area of America. Then Holland was the center of the world just like the Italy was in the previous century. New York City was once called New Amsterdam when Dutch merchants landed and established colonies. Among them, Henry Hudson is probably the most recognized individual in the history of New York City today. “This small island is inhabited by two major creatures which we do not have in our homeland. The one creature is a large arthropod made of three body segments: the frontal segment resembles a horseshoe, the middle segment resembles a spiny crab and its tail resembles a sharp sword. Although they gather beaches here in great numbers, they are not edible due to their extremely offensive odor. Another creature which is abundant here, has the head of wild rabbit. This animal of great swimming ability has frontal legs resemble the webbed feet of a duck. The bottom half of the body resembles that of a seal. This docile rabbit of the sea is easy to catch as it does not fear people. The larger male sea rabbits control harems of 20 to 25 females. The meat of the sea rabbit is very tender and tasty.” This is what Hadson wrote in his personal journal in 1609 about the horseshoe crab and the sea rabbit in today’s Coney Island area of Brooklyn, New York. Sadly, just like the Dodo bird and the Thylacine, the sea rabbit was driven to extinction by the European settlers’ greed. When Dutch merchants and traders arrived here, sea rabbits were one of the first animals they hunted down to bring their furs to homeland to satisfy the fur craze of the time. To increase the shipment volume of furs of sea rabbit and beavers from New Amsterdam, Dutch merchants also started using wampum (beads made of special clam shells) as the first official currency of this country.

 

At the North Eastern shores of the United States, two species of sea rabbits were commonly found. They are Coney Island Sea Rabbit (Monafluffchus americanus) and Coney Island Tiger-striped Sea Rabbit (Monafluffchus konjinicus). Sadly, due to their over harvesting in the previous centuries, their conservation status became “Extinct in the Wild” (ET) in the Red List Endangered species by the International Union for Conservation of Nature (IUCN). Currently, these sea rabbits are only found at breeding centers at selected zoos and universities such as Coney Island Aquarium and Coney Island University in Brooklyn, New York. The one shown in this photograph was named "Seara" and has been cared by Dr. Takeshi Yamada at Coney Island University.

 

The sea rabbit is one of the families of the Pinniped order. Pinnipeds (from Latin penna = flat and pes/pedis = foot) are sea-mammals: they are homeothermic (i.e having high and regulated inner temperature), lung-breathing (i.e dependant on atmospheric oxygen) animals having come back to semi aquatic life. As soon as they arrive ashore, females are caught by the nearest adult male. Males can maintain harems of about 20 females on average. Several hours to several days after arriving ashore, pregnant females give birth to eight to ten pups with a dark brown fur. As soon as birth occurs, the mother’s special smell and calls help her pups bond specifically to her. The mother stays ashore with her pup for about one week during which the pup gains weight. During the first week spent with her newborn, the mother becomes receptive. She will be impregnated by the bull, which control the harem. Implantation of the embryo will occur 3 months later, in March-April. During the reproductive period, the best males copulate with several tens females. To do so, males have to stay ashore without feeding in order to keep their territory and their harem. In mid-January, when the last females have been fecundated, males leave at sea to feed. Some of them will come back later in March-April for the moult. The other ones will stay at sea and will come back on Coney Island only in next November. After fecundation, the mother goes at sea for her first meal. At sea, mothers feed on clams, crabs, shrimps, fish (herring, anchovy, Pollock, capelin etc.) and squids. When she is back, the mother recovers her pups at the beach she left them. Suckling occurs after auditive and olfactory recognition had occured. In March-April, the dark brown fur is totally replaced by an adult-like light brownish grey fur during the moult that lasts 1-2 months. This new fur is composed by 2 layers. Externally, the guard fur is composed by flat hairs that recover themselves when wet. By doing so, they make a water-proof barrier for the under fur. The underfur retains air when the seal is dry. Because of isolating properties of the air, the underfur is the insulating system of the fur. In March-April, the fur of adults is partially replaced. First reproduction occurs at 1-yr old in females. Males are physiologically matures at 1 year old but socially matures at +2 years old.

 

NOTE: The name of Coney Island is commonly thought to be derived from the Dutch Konijn Eylandt or Rabbit Island as apparently the 17th century European settlers noted many rabbits running amuck on the island.

 

www.takeshiyamada.weebly.com/performances.html

 

www.takeshiyamada.weebly.com/sea-rabbit-center.html

 

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www.flickr.com/photos/searabbits23/

 

www.flickr.com/photos/searabbit22

 

www.flickr.com/photos/searabbit021/

 

www.flickr.com/photos/searabbit20

 

www.flickr.com/photos/searabbit19

 

www.flickr.com/photos/searabbit18

 

www.flickr.com/photos/searabbit17

 

www.flickr.com/photos/searabbit16

 

www.flickr.com/photos/searabbit15

 

www.flickr.com/photos/searabbit14

 

www.flickr.com/photos/searabbit13

 

www.flickr.com/photos/searabbit12

 

www.flickr.com/photos/searabbit11

 

www.flickr.com/photos/searabbit10

 

www.flickr.com/photos/searabbit9

 

www.flickr.com/photos/searabbit8

 

www.flickr.com/photos/searabbit7

 

www.flickr.com/photos/searabbit6

 

www.flickr.com/photos/searabbit5

 

www.flickr.com/photos/searabbit4

 

www.flickr.com/photos/searabbit3

 

www.flickr.com/photos/searabbit2

 

www.flickr.com/photos/searabbit1

 

www.flickr.com/photos/diningwithsearabbits03

 

www.flickr.com/photos/diningwithsearabbits02

 

www.flickr.com/photos/diningwithsearabbits01

 

www.flickr.com/photos/yamadaimmortalized2/

 

www.flickr.com/photos/takeshiyamadaimmortalized/

 

www.flickr.com/photos/yamadabellhouse2014/

 

www.flickr.com/photos/museumofworldwonders3/

 

www.flickr.com/photos/museumofworldwonders2

 

www.flickr.com/photos/museumofworldwonders/

 

www.flickr.com/photos/takeshiyamadapaintings/

 

===========================================

 

For any questions, please email contact Takeshi Yamada, Art & Rogue Taxidermy, Museum of World Wonders, official website. www.takeshiyamada.weebly.com/

 

================================================

 

www.takeshiyamada.weebly.com

 

For any questions, please contact Dr. Takeshi Yamada. His email address is posted in the chapter page (the last page or the first page).

 

(Updated April 7B, 2015)

Progress build up around these protected species. Nearly extinct over 10 years ago they are protected and loved.

Taken from Blackford Hill. Looks a nice day, but shortly after taking this it started pelting down with hail, in true Edinburgh style.

Superdomain: Neomura

Domain: Eukaryota

(unranked): Unikonta

(unranked): Obazoa

(unranked): Opisthokonta

(unranked) Holozoa

(unranked) Filozoa

Kingdom: Animalia

Subkingdom: Eumetazoa

(unranked): Bilateria

(unranked): Protostomia

Superphylum: Lophotrochozoa

Phylum: Mollusca

Subphylum: Conchifera

Class: Cephalopoda

Subclass: Coleoidea

Cohort: Neocoleoidea

Superorder: Octopodiformes

Order: Octopoda

Suborder: †Teudopseina

Superfamily: †Muensterelloidea

Family: †Muensterellidae

Subfamily: †Enchoteuthinae

Genus: †Tusoteuthis

Species: †T. longa

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Superdomain: Neomura

Domain: Eukaryota

(unranked): Unikonta

(unranked): Obazoa

(unranked): Opisthokonta

(unranked) Holozoa

(unranked) Filozoa

Kingdom: Animalia

Subkingdom: Eumetazoa

Clade: ParaHoxozoa

Clade: Bilateria

Clade: Nephrozoa

Superphylum: Deuterostomia

Phylum: Chordata

Clade: Olfactores

Subphylum: Vertebrata

Infraphylum: Gnathostomata

Clade: Eugnathostomata

Class: Chondrichthyes

Subclass: Elasmobranchii

Infraclass: Euselachii

Superorder: Squalomorphii

Order: Hexanchiformes

Family: Hexanchidae

Genus: Hexanchus

Species: H. gracilis†

Superdomain: Neomura

Domain: Eukaryota

(unranked): Unikonta

(unranked): Obazoa

(unranked): Opisthokonta

(unranked) Holozoa

(unranked) Filozoa

Kingdom: Animalia

Subkingdom: Eumetazoa

(unranked): Bilateria

Superphylum: Deuterostomia

Phylum: Chordata

Subphylum: Vertebrata

Infraphylum: Gnathostomata

Superclass: Osteichthyes

Clade: Sarcopterygii

Class: Dipnoi

Order: Ceratodontiformes

Family: †Ceratodontidae

Genus: †Ariguna

Species: †A. formosa

Perpignan (66): les sapeurs pompiers s'entrainent a gerer une fuite de gaz en procédant au pincement et extinction

Superdomain: Neomura

Domain: Eukaryota

Clade: Amorphea

(unranked): Obazoa

(unranked): Opisthokonta

(unranked) Holozoa

(unranked) Filozoa

Clade: Choanozoa

Kingdom: Animalia

Subkingdom: Eumetazoa

Clade: ParaHoxozoa

Clade: Bilateria

Clade: Nephrozoa

Superphylum: Deuterostomia

Phylum: Chordata

Clade: Olfactores

Subphylum: Vertebrata

Infraphylum: Gnathostomata

Clade: Eugnathostomata

Clade: Teleostomi

Superclass: Tetrapoda

Clade: Reptiliomorpha

Clade: Amniota

Class: Mammalia

Clade: Theriimorpha

Clade: Theriiformes

Clade: Trechnotheria

Clade: Cladotheria

Clade: Zatheria

Clade: Tribosphenida

Clade: Eutheria

Infraclass: Placentalia

Clade: Exafroplacentalia

Magnorder: Boreoeutheria

Superorder: Laurasiatheria

(unranked): Scrotifera

Grandorder: Ferungulata

Clade: Ungulata

Order: Artiodactyla

Clade: Artiofabula

Clade: Cetruminantia

Clade: Cetancodontamorpha

Suborder: Whippomorpha

Clade: Cetaceamorpha

Infraorder: Cetacea

Parvorder: Mysticeti

Superfamily: Physeteroidea

Family: Physeteridae

Genus: †Idiorophus

Species: †I. patagonicus

The Glyptodon specimen in the main hall of London's Natural History Museum

THE FAIRY CHIMNEYS

  

Cappadocia - World Heritage List.

 

whc.unesco.org/en/list/357

 

In a spectacular landscape, entirely sculpted by erosion, the Göreme valley and its surroundings contain rock-hewn sanctuaries that provide unique evidence of Byzantine art in the post-Iconoclastic period. Dwellings, troglodyte villages and underground towns – the remains of a traditional human habitat dating back to the 4th century – can also be seen there.

Brief synthesis

Located on the central Anatolia plateau within a volcanic landscape sculpted by erosion to form a succession of mountain ridges, valleys and pinnacles known as “fairy chimneys” or hoodoos, Göreme National Park and the Rock Sites of Cappadocia cover the region between the cities of Nevşehir, Ürgüp and Avanos, the sites of Karain, Karlık, Yeşilöz, Soğanlı and the subterranean cities of Kaymaklı and Derinkuyu. The area is bounded on the south and east by ranges of extinct volcanoes with Erciyes Dağ (3916 m) at one end and Hasan Dağ (3253 m) at the other. The density of its rock-hewn cells, churches, troglodyte villages and subterranean cities within the rock formations make it one of the world's most striking and largest cave-dwelling complexes. Though interesting from a geological and ethnological point of view, the incomparable beauty of the decor of the Christian sanctuaries makes Cappadocia one of the leading examples of the post-iconoclastic Byzantine art period.

It is believed that the first signs of monastic activity in Cappadocia date back to the 4th century at which time small anchorite communities, acting on the teachings of Basileios the Great, Bishop of Kayseri, began inhabiting cells hewn in the rock. In later periods, in order to resist Arab invasions, they began banding together into troglodyte villages or subterranean towns such as Kaymakli or Derinkuyu which served as places of refuge.

Cappadocian monasticism was already well established in the iconoclastic period (725-842) as illustrated by the decoration of many sanctuaries which kept a strict minimum of symbols (most often sculpted or tempera painted crosses). However, after 842 many rupestral churches were dug in Cappadocia and richly decorated with brightly coloured figurative painting. Those in the Göreme Valley include Tokalı Kilise and El Nazar Kilise (10th century), St. Barbara Kilise and Saklı Kilise (11th century) and Elmalı Kilise and Karanlık Kilise (end of the 12th – beginning of the 13th century).

Criterion (i): Owing to their quality and density, the rupestral sanctuaries of Cappadocia constitute a unique artistic achievement offering irreplaceable testimony to the post-iconoclastic Byzantine art period.

Criterion (iii): The rupestral dwellings, villages, convents and churches retain the fossilized image of a province of the Byzantine Empire between the 4th century and the arrival of the Seljuk Turks (1071). Thus, they are the essential vestiges of a civilization which has disappeared.

Criterion (v): Cappadocia is an outstanding example of a traditional human settlement which has become vulnerable under the combined effects of natural erosion and, more recently, tourism.

Criterion (vii): In a spectacular landscape dramatically demonstrating erosional forces, the Göreme Valley and its surroundings provide a globally renowned and accessible display of hoodoo landforms and other erosional features, which are of great beauty, and which interact with the cultural elements of the landscape.

Integrity

Göreme National Park and the Rock Sites of Cappadocia, having been extensively used and modified by man for centuries, is a landscape of harmony combining human interaction and settlement with dramatic natural landforms. There has been some earthquake damage to some of the cones and the pillars, but this is seen as a naturally occurring phenomenon. Overuse by tourists and some vandalism have been reported and some incompatible structures have been introduced.

The erosional processes that formed the distinctive conical rock structures will continue to create new fairy chimneys and rock pillars, however due to the rate of this process, the natural values of the property may still be threatened by unsustainable use. The cultural features, including rock-hewn churches and related cultural structures, mainly at risk of being undermined by erosion and other negative natural processes coupled with mass tourism and development pressures, can never be replaced. threats Some of the churches mentioned by early scholars such as C. Texier, H.G. Rott and Guillaume de Jerphanion are no longer extant.

Authenticity

The property meets the conditions of authenticity as its values and their attributes, including its historical setting, form, design, material and workmanship adequately reflect the cultural and natural values recognized in the inscription criteria.

Given the technical difficulties of building in this region, where it is a matter of hewing out structures within the natural rock, creating architecture by the removal of material rather than by putting it together to form the elements of a building, the underlying morphological structure and the difficulties inherent in the handling of the material inhibited the creative impulses of the builders. This conditioning of human effort by natural conditions persisted almost unchanged through successive periods and civilizations, influencing the cultural attitudes and technical skills of each succeeding generation.

Protection and management requirements

The World Heritage property Göreme National Park and the Rock Sites of Cappadocia is subject to legal protection in accordance with both the Protection of Cultural and Natural Resources Act No. 2863 and the National Parks Act No. 2873. The entire territory between the cities of Nevşehir, Ürgüp and Avanos is designated as a National Park under the Act No. 2873. In addition, natural, archaeological, urban, and mixed archaeological and natural conservation areas, two underground towns, five troglodyte villages, and more than 200 individual rock-hewn churches, some of which contain numerous frescoes, have been entered into the register of immovable monuments and sites according to the Act No. 2863.

Legal protection, management and monitoring of the Göreme National Park and the Rock Sites of Cappadocia fall within the scope of national and regional governmental administrations. The Nevşehir and Kayseri Regional Conservation Councils are responsible for keeping the register of monuments and sites, including carrying out all tasks related to the legal protection of monuments and listed buildings and the approval to carry out any restoration-related works. They also evaluate regional and conservation area plans prepared by the responsible national and/or local (i.e. municipal) authorities.

Studies for revision and updating of the existing land use and conservation plan (Göreme National Park Long-term Development Plan) of 1981 were completed in 2003. The major planning decisions proposed were that natural conservation areas are to be protected as they were declared in 1976. Minor adjustments in the peripheral areas of settlements and spatial developments of towns located in the natural conservation sites including Göreme, Ortahisar, Çavuşin, Ürgüp and Mustafapaşa will be strictly controlled. In other words, the Plan proposes to confine the physical growth of these towns to recently established zones. Hotel developments will take into account the set limits for room capacities. Furthermore, the plan also suggested that local authorities should be advised to review land use decisions for areas that have been reserved for tourism developments in the town plans.

Preparation of conservation area plans for the urban and/or mixed urban-archaeological conservation sites within the historic sections of Göreme are in place and provide zoning criteria and the rules and guidelines to be used in the maintenance and restoration of listed buildings and other buildings which are not registered, but which are located within the historic zones. Similar planning studies for the towns of Ortahisar and Uçhisar are in place. Once finalised, a conservation area plan for the urban conservation area in Ürgüp will be in place. All relevant plans are kept up to date on a continuing basis.

Appropriate facilities aimed at improving the understanding of the World Heritage property have been completed for the subterranean towns of Kaymaklı and Derinkuyu, and are required for Göreme and Paşabağı.

Monuments in danger due to erosion, including the El Nazar, Elmalı, and Meryemana (Virgin Mary) churches, have been listed as monuments requiring priority action. Specific measures for their protection, restoration and maintenance are required at the site level.

While conservation plans and protection measures are in place for individual sites, it is recognised by the principal parties responsible for site management that an integrated Regional Plan for the Cappadocia Cultural and Tourism Conservation and Development Area is required to protect the World Heritage values of the property. Adequate financial, political and technical support is also required to secure the management of the property.

 

whc.unesco.org/en/list/357

  

www.nationalgeographic.com/travel/world-heritage/cappadocia/

 

Long dormant volcano. Budj Bim is the source of the Tyrendarra lava flow which extends over 50km to the southwest. It is central to the history of the Gunditjmara people.

 

Mount Eccles National Park is Victoria’s first co-managed national park. The park is managed by Gunditjmara Traditional Owners and Parks Victoria.

 

The park’s tranquil crater lake and pleasant bushland surrounds make it a pleasant place for picnicking, camping and bushwalking. Nature trails follow the old crater rim.

The Extinct play AFU

Extinct volcano and lava flow surrounds the 1737 church at Tepanco, Mexico taken on Kodachrome on 1 August, 1971.

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