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Absolutely no photoshopping involved here! This was taken in our garden looking towards Eastbourne.
In meteorology, a cloud is an aerosol comprising a visible mass of minute liquid droplets, frozen crystals, or particles suspended in the atmosphere above the surface of a planetary body. The droplets and crystals may be made of water or various chemicals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere (which includes the troposphere, stratosphere, and mesosphere). Nephology is the science of clouds which is undertaken in the cloud physics branch of meteorology.
There are two methods of naming clouds in their respective layers of the atmosphere; Latin and common. Cloud types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adaptation of Luke Howard's nomenclature. Formally proposed in 1802, it became the basis of a modern international system that divides clouds into five physical forms that appear in any or all of three altitude levels (formerly known as étages). These physical types, in approximate ascending order of convective activity, include stratiform sheets, cirriform wisps and patches, stratocumuliform layers (mainly structured as rolls, ripples, and patches), cumuliform heaps, and very large cumulonimbiform heaps that often show complex structure. The physical forms are divided by altitude level into ten basic genus-types. The Latin names for applicable high-level genera carry a cirro- prefix, and an alto- prefix is added to the names of the mid-level genus-types. Most of the genera can be subdivided into species and further subdivided into varieties.
Two cirriform clouds that form higher up in the stratosphere and mesosphere have common names for their main types. They are seen infrequently, mostly in the polar regions of Earth. Clouds have been observed in the atmospheres of other planets and moons in the Solar System and beyond. However, due to their different temperature characteristics, they are often composed of other substances such as methane, ammonia, and sulfuric acid as well as water.
Taken as a whole, homospheric clouds can be cross-classified by form and level to derive the ten tropospheric genera and the two additional major types above the troposphere. The cumulus genus includes three species that indicate vertical size. Clouds with sufficient vertical extent to occupy more than one altitude level are officially classified as low- or mid-level according to the altitude range at which each initially forms. However they are also more informally classified as multi-level or vertical.
For further information please visit
In meteorology, a cloud is an aerosol comprising a visible mass of minute liquid droplets, frozen crystals, or particles suspended in the atmosphere above the surface of a planetary body. The droplets and crystals may be made of water or various chemicals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere (which includes the troposphere, stratosphere, and mesosphere). Nephology is the science of clouds which is undertaken in the cloud physics branch of meteorology.
There are two methods of naming clouds in their respective layers of the atmosphere; Latin and common. Cloud types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adaptation of Luke Howard's nomenclature. Formally proposed in 1802, it became the basis of a modern international system that divides clouds into five physical forms that appear in any or all of three altitude levels (formerly known as étages). These physical types, in approximate ascending order of convective activity, include stratiform sheets, cirriform wisps and patches, stratocumuliform layers (mainly structured as rolls, ripples, and patches), cumuliform heaps, and very large cumulonimbiform heaps that often show complex structure. The physical forms are divided by altitude level into ten basic genus-types. The Latin names for applicable high-level genera carry a cirro- prefix, and an alto- prefix is added to the names of the mid-level genus-types. Most of the genera can be subdivided into species and further subdivided into varieties.
Two cirriform clouds that form higher up in the stratosphere and mesosphere have common names for their main types. They are seen infrequently, mostly in the polar regions of Earth. Clouds have been observed in the atmospheres of other planets and moons in the Solar System and beyond. However, due to their different temperature characteristics, they are often composed of other substances such as methane, ammonia, and sulfuric acid as well as water.
Taken as a whole, homospheric clouds can be cross-classified by form and level to derive the ten tropospheric genera and the two additional major types above the troposphere. The cumulus genus includes three species that indicate vertical size. Clouds with sufficient vertical extent to occupy more than one altitude level are officially classified as low- or mid-level according to the altitude range at which each initially forms. However they are also more informally classified as multi-level or vertical.
For further information please visit
Damselfly or water damselfly (Zygoptera) is a suborder of the dragonflies (Odonata), which are subdivided into 19 families with about 2600 species.
Head to head with a Bald Eagle - Rocamadour - Lot - Occitanie - France - Europe
Le Pygargue à tête blanche (Haliaeetus leucocephalus) est une espèce de rapaces qui vit en Amérique du Nord.
Malgré son nom anglais de Bald Eagle (« aigle chauve ») ou sa dénomination populaire d'« aigle à tête blanche », il ne s'agit pas d'un aigle du genre Aquila mais d'un pygargue du genre Haliaeetus : il s'en distingue par son régime alimentaire, essentiellement composé de poissons, mais aussi par son bec massif et par le fait que ses pattes ne sont pas recouvertes de plumes jusqu'aux serres, l'un des caractères propres aux vrais aigles. Alors que l'aigle vit dans les massifs forestiers et les montagnes, le pygargue préfère les lacs, les rivières et les zones côtières, où il peut trouver sa nourriture. À ce titre, il est parfois nommé « aigle de mer » ou « aigle pêcheur » américain.
Subdivisé en deux sous-espèces, il se rencontre sur presque toute la superficie de l'Amérique du Nord, de l'Alaska au nord jusqu'au Mexique au sud tant sur la côte Atlantique que Pacifique.
Emblème national des États-Unis, l'espèce a été un temps menacée dans ce pays au XXe siècle.
Source Wikipedia
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The Bald Eagle (Haliaeetus leucocephalus) is a species of raptor that lives in North America.
Despite its English name of Bald Eagle (“bald eagle”) or its popular name of “white-headed eagle”, it is not an eagle of the genus Aquila but a sea eagle of the genus Haliaeetus: it is It is distinguished by its diet, essentially composed of fish, but also by its massive beak and by the fact that its legs are not covered with feathers up to the talons, one of the characteristics specific to true eagles. While the eagle lives in forests and mountains, the sea eagle prefers lakes, rivers and coastal areas, where it can find its food. As such, it is sometimes referred to as the American "sea eagle" or "fish eagle".
Subdivided into two subspecies, it is found over almost the entire surface of North America, from Alaska in the north to Mexico in the south on both the Atlantic and Pacific coasts.
The national emblem of the United States, the species was once threatened in this country in the 20th century.
Source Wikipedia
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Karaca Cave (Turkish: Karaca Mağarası) is a network of caves located near the town of Torul in Gümüşhane Province, Turkey.
In the area extending between Gümüşhane and Torul, there are extensive formations consisting of various types of extrusive, igneous rock, including andesitic and basaltic lavas, tuffs and agglomerates. The total thickness of these deposits reaches 1,000 m (3,300 ft). These igneous strata are interleaved with sedimentary layers, varying in thickness between 100 and 200 m (330 and 660 ft) and consisting of limestone and certain other types of sedimentary rock. The Karaca Cave formed in one of these layers of highly-fissured, massive limestone sandwiched between volcanics.
Karaca Cave is rich in dripstone formations of many different shapes and colours, including stalactites, stalagmites, and travertines. There are also many cave roses located on certain of the travertines and stalagmites.
Some of the dripstone pools are very large - particularly those in the inner parts of the cave, which range up to 1 m (3.3 ft) in depth.
The travertines vary in colour from white to dark blue, revealing the presence of high levels of iron and magnesium minerals in the cave waters.
The cave system is disposed more or less in a level plane and consists of four interconnected caverns. Two of these caverns are further subdivided by 'walls' composed of dripstone, and it could thus be argued that Karaca comprises not four but six chambers.
The height of the cave entrance is about 1.8 m (5.9 ft) - the height of an average man - but, as one moves deeper into the interior increases steadily, the cave opening out into a funnel shape. The cave is roughly 105 m (344 ft) in length, averages 18 m (59 ft) in height and has a total floor area of 1,500 m2 (16,000 sq ft).
There is no stream in Karaca, water percolating through fissures in the roof of the cave being responsible for the formation of the dripstones. Such water as persists within the cave is in the form of various ponds and pools. The ponds at the entrance of the third and fourth caverns contain a considerable volume of water.
There is no significant air circulation in the cave, with the result that the level of humidity in its atmosphere increases from around 65% at the entrance to up to 75% in the cave's interior. The air inside the cave is cooler than that outside it in summertime and warmer in winter. Because of this, it is considered to have a microclimate of its own.
The Karaca Cave has been open to visitors since 1996.
Siberian huskies sled dog team at the Polar Adventure : Méaudre, Isere, France
This sport takes back ancestral traditions which allowed the Inuits to survive in the big Arctic deserts and represent the link with the nature.
The sled dog racing is subdivided into several categories according to the number of dogs harnessed and in three subcategories according to the breed of dogs harnessed.
Indeed, the faster Siberian Husky compete in a separate category, the other three breeds : Alaskan Malamute, Samoyed and Greenland dog run in the same category, while the so-called "Nordic type" dogs participate in their own category.
In 1910 stock broker William Porter built the colossal granite mansion “Foxcroft” on the top of Fox Hill, selected for the commanding views it afforded. In 1911, while traveling back to New York after a weekend at Foxcroft, Porter was killed in an automobile accident. He was survived by his wife Ruth Halliwell Porter, who was returning from a European vacation aboard the Lusitania at the time of the crash.
In 1913, Ruth married Warren Van Slyke and renamed their part-time retreat the Van Slyke Castle. When Warren died in 1925, Ruth moved to the castle permanently and remained there until her death in 1940. On March 1, 1949, the Castle was purchased by Celeste and Robin MacFadden, who subsequently sold to Suzanne S. Christie on July 2, 1951. Between 1951 and 1962, Suzanne S. Christie was to become Suzanne S. O’Sullivan then Suzanne Noyes Brussel. As strange as it may seem, Suzanne (who was the sole owner) abandoned the mansion between husbands, and left it to the mercy of the elements. In 1959, the magnificent structure was reduced to ruins in a fire of undetermined origin.
On August 18, 1978, Suzanne Brussel sold the ruins to Bruce Ademski of the Ademski and Van Saun Home Improvement Company. Ademski then subdivided the 15.9 acre parcel into three 5 acre lots. On February 22, 1980 the State of New Jersey filed a “Declaration of Taking;” which informed Ademski that his lots would soon be seized by the NJDEP at a non-negotiable price. Shortly after the receipt of this document, Ademski’s lots became part of Ramapo Mountain State Forest.
In the early part of the 20th century, Clifford MacEvoy purchased about 2600-acres of what would become Ramapo Mountain State Forest. In 1976 the area became state lands using Green Acres and federal funds. The majority of Park acreage was conveyed by the trustee of the Clifford MacEvoy estate to the State of New Jersey to be included as part of the existing Ramapo State Forest.
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Damselfly or water damselfly (Zygoptera) is a suborder of the dragonflies (Odonata), which are subdivided into 19 families with about 2600 species.
The chain is a unit of length equal to 66 feet (22 yards). It is subdivided into 100 links This is the handle and linkage of the chain used many years ago to measure allotment plots.
In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body or similar space. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere, which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology. There are two methods of naming clouds in their respective layers of the homosphere, Latin and common. Genus types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adoption of Luke Howard's nomenclature that was formally proposed in 1802. It became the basis of a modern international system that divides clouds into five physical forms which can be further divided or classified into altitude levels to derive ten basic genera. The main representative cloud types for each of these forms are stratus, cirrus, stratocumulus, cumulus, and cumulonimbus. Low-level clouds do not have any altitude-related prefixes. However mid-level stratiform and stratocumuliform types are given the prefix alto- while high-level variants of these same two forms carry the prefix cirro-. Genus types with sufficient vertical extent to occupy more than one level do not carry any altitude related prefixes. They are classified formally as low- or mid-level depending on the altitude at which each initially forms, and are also more informally characterized as multi-level or vertical. Most of the ten genera derived by this method of classification can be subdivided into species and further subdivided into varieties. Very low stratiform clouds that extend down to the Earth's surface are given the common names fog and mist, but have no Latin names. 65518
The Polar Adventure : Méaudre, Isere, France
This sport takes back ancestral traditions which allowed the Inuits to survive in the big Arctic deserts and represent the link with the nature.
The sled dog racing is subdivided into several categories according to the number of dogs harnessed and in three subcategories according to the breed of dogs harnessed.
Indeed, the faster Siberian Husky compete in a separate category, the other three breeds : Alaskan Malamute, Samoyed and Greenland dog run in the same category, while the so-called "Nordic type" dogs participate in their own category.
Damselfly or water damselfly (Zygoptera) is a suborder of the dragonflies (Odonata), which are subdivided into 19 families with about 2600 species.
Damselfly or water damselfly (Zygoptera) is a suborder of the dragonflies (Odonata), which are subdivided into 19 families with about 2600 species.
Absolutely no manipulation involved! This cloud looks as if it has been bent out of shape and was hovering near my brother's property in Orange, New South Wales. And if you would like to hear Amen Corner's version of 'Bend Me, Shape Me' visit www.youtube.com/watch?v=74sUIFY9vFQ.
In meteorology, a cloud is an aerosol comprising a visible mass of minute liquid droplets, frozen crystals, or particles suspended in the atmosphere above the surface of a planetary body. The droplets and crystals may be made of water or various chemicals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere (which includes the troposphere, stratosphere, and mesosphere). Nephology is the science of clouds which is undertaken in the cloud physics branch of meteorology.
There are two methods of naming clouds in their respective layers of the atmosphere; Latin and common. Cloud types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adaptation of Luke Howard's nomenclature. Formally proposed in 1802, it became the basis of a modern international system that divides clouds into five physical forms that appear in any or all of three altitude levels (formerly known as étages). These physical types, in approximate ascending order of convective activity, include stratiform sheets, cirriform wisps and patches, stratocumuliform layers (mainly structured as rolls, ripples, and patches), cumuliform heaps, and very large cumulonimbiform heaps that often show complex structure. The physical forms are divided by altitude level into ten basic genus-types. The Latin names for applicable high-level genera carry a cirro- prefix, and an alto- prefix is added to the names of the mid-level genus-types. Most of the genera can be subdivided into species and further subdivided into varieties.
Two cirriform clouds that form higher up in the stratosphere and mesosphere have common names for their main types. They are seen infrequently, mostly in the polar regions of Earth. Clouds have been observed in the atmospheres of other planets and moons in the Solar System and beyond. However, due to their different temperature characteristics, they are often composed of other substances such as methane, ammonia, and sulfuric acid as well as water.
Taken as a whole, homospheric clouds can be cross-classified by form and level to derive the ten tropospheric genera and the two additional major types above the troposphere. The cumulus genus includes three species that indicate vertical size. Clouds with sufficient vertical extent to occupy more than one altitude level are officially classified as low- or mid-level according to the altitude range at which each initially forms. However they are also more informally classified as multi-level or vertical.
For further information please visit
In meteorology, a cloud is an aerosol comprising a visible mass of minute liquid droplets, frozen crystals, or particles suspended in the atmosphere above the surface of a planetary body. The droplets and crystals may be made of water or various chemicals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere (which includes the troposphere, stratosphere, and mesosphere). Nephology is the science of clouds which is undertaken in the cloud physics branch of meteorology.
There are two methods of naming clouds in their respective layers of the atmosphere; Latin and common. Cloud types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adaptation of Luke Howard's nomenclature. Formally proposed in 1802, it became the basis of a modern international system that divides clouds into five physical forms that appear in any or all of three altitude levels (formerly known as étages). These physical types, in approximate ascending order of convective activity, include stratiform sheets, cirriform wisps and patches, stratocumuliform layers (mainly structured as rolls, ripples, and patches), cumuliform heaps, and very large cumulonimbiform heaps that often show complex structure. The physical forms are divided by altitude level into ten basic genus-types. The Latin names for applicable high-level genera carry a cirro- prefix, and an alto- prefix is added to the names of the mid-level genus-types. Most of the genera can be subdivided into species and further subdivided into varieties.
Two cirriform clouds that form higher up in the stratosphere and mesosphere have common names for their main types. They are seen infrequently, mostly in the polar regions of Earth. Clouds have been observed in the atmospheres of other planets and moons in the Solar System and beyond. However, due to their different temperature characteristics, they are often composed of other substances such as methane, ammonia, and sulfuric acid as well as water.
Taken as a whole, homospheric clouds can be cross-classified by form and level to derive the ten tropospheric genera and the two additional major types above the troposphere. The cumulus genus includes three species that indicate vertical size. Clouds with sufficient vertical extent to occupy more than one altitude level are officially classified as low- or mid-level according to the altitude range at which each initially forms. However they are also more informally classified as multi-level or vertical.
For further information please visit en.wikipedia.org/wiki/Cloud
In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body or similar space. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere, which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology. There are two methods of naming clouds in their respective layers of the homosphere, Latin and common. Genus types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adoption of Luke Howard's nomenclature that was formally proposed in 1802. It became the basis of a modern international system that divides clouds into five physical forms which can be further divided or classified into altitude levels to derive ten basic genera. The main representative cloud types for each of these forms are stratus, cirrus, stratocumulus, cumulus, and cumulonimbus. Low-level clouds do not have any altitude-related prefixes. However mid-level stratiform and stratocumuliform types are given the prefix alto- while high-level variants of these same two forms carry the prefix cirro-. Genus types with sufficient vertical extent to occupy more than one level do not carry any altitude related prefixes. They are classified formally as low- or mid-level depending on the altitude at which each initially forms, and are also more informally characterized as multi-level or vertical. Most of the ten genera derived by this method of classification can be subdivided into species and further subdivided into varieties. Very low stratiform clouds that extend down to the Earth's surface are given the common names fog and mist, but have no Latin names. 65633
Sprawling on the fringes of the city
In geometric order
An insulated border
In between the bright lights
And the far unlit unknown
Growing up it all seems so one-sided
Opinions all provided
The future pre-decided
Detached and subdivided
In the mass production zone
Nowhere is the dreamer
Or the misfit so alone
(Subdivisions)
In the high school halls
In the shopping malls
Conform or be cast out
(Subdivisions)
In the basement bars
In the backs of cars
Be cool or be cast out
Naples Botanical Gardens
60 Acre Wildlife Reserve
Naples, FL
The anhinga (Anhinga anhinga), sometimes called snakebird, darter, American darter, or water turkey, is a water bird of the warmer parts of the Americas. The word anhinga comes from the Brazilian Tupi language and means devil bird or snake bird. The origin of the name snakebird is apparent when swimming: only the colored neck appears above water so the bird looks like a snake ready to strike. They do not have external nares (nostrils) and breathe solely through their epiglottis.
The anhinga is placed in the darter family, Anhingidae, and is closely related to Indian (Anhinga melanogaster), African (Anhinga rufa), and Australian (Anhinga novaehollandiae) darters. Like other darters, the anhinga hunts by spearing fish and other small prey using its sharp, slender beak.
Anhinga species are found all over the world in warm shallow waters. The American anhinga has been subdivided into two subspecies, A. a. anhinga and A. a. leucogaster, based on their location. A. a. leucogaster can be found in the southern United States, Mexico, Cuba, and Grenada. A fossil species Anhinga walterbolesi has been described from the Late Oligocene to Early Miocene of Australia.
Only birds that live in the extreme north and south of their range migrate and do so based on temperature and available sunlight. Anhingas will migrate towards the equator during winter but this range is "determined by the amount of sunshine to warm the chilled birds". Although not in their usual range, anhingas have been found as far north as the states of Pennsylvania and Wisconsin in the United States. – Wikipedia
Prambanan, of Yogyakarta, Indonesia, is known for a large, nearby complex of temples built in the 9th and 10th centuries. The best-known set of temples in the complex is that of Lara Jonggrang, also called Candi Prambanan (Prambanan Temple) because of its close proximity to the village. These temples were designated a UNESCO World Heritage site in 1999.
The Lara Jonggrang was said to have been built by Dhaksa, a king of Mendang-Mataram (Hindu-Mataram) in the early 10th century, to worship the Hindu god Shiva. It is the largest Shiva temple in Indonesia. Lara Jonggrang, meaning Slender Maiden, was the name given by the people of the neighbourhood to a large statue of the Hindu goddess Durga (wife of Shiva) in the temple. The Lara Jonggrang was built on a four-square plane, surrounded by four walls with four large gates. The temples are subdivided into a higher and a lower terrace. On the higher terrace are major temples of Shiva, Vishnu, and Brahma with three smaller temples of their animal vehicles. The temples of the gods are decorated with reliefs depicting the Ramayana, one of the great Hindu epics. On the lower terrace are four sets of smaller temples surrounded by an inner wall with four gates.
Siberian Huskies at Retordica, Plateau de Retord, Cuvéry, Ain, France
For more than 25 years, an international dog sled race has been taking place in the wilderness of Plateau de Retord. Many mushers love this site to train their teams throughout the winter.
The sled dog racing is subdivided into several categories according to the number of dogs harnessed and in three subcategories according to the breed of dogs harnessed.
Indeed, the faster Siberian Husky compete in a separate category, the other three breeds : Alaskan Malamute, Samoyed and Greenland dog run in the same category, while the so-called "Nordic type" dogs participate in their own category.
The Polar Adventure : Méaudre, Isere, France
This sport takes back ancestral traditions which allowed the Inuits to survive in the big Arctic deserts and represent the link with the nature.
The sled dog racing is subdivided into several categories according to the number of dogs harnessed and in three subcategories according to the breed of dogs harnessed.
Indeed, the faster Siberian Husky compete in a separate category, the other three breeds : Alaskan Malamute, Samoyed and Greenland dog run in the same category, while the so-called "Nordic type" dogs participate in their own category.
In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body or similar space. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere, which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology. There are two methods of naming clouds in their respective layers of the homosphere, Latin and common. Genus types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adoption of Luke Howard's nomenclature that was formally proposed in 1802. It became the basis of a modern international system that divides clouds into five physical forms which can be further divided or classified into altitude levels to derive ten basic genera. The main representative cloud types for each of these forms are stratus, cirrus, stratocumulus, cumulus, and cumulonimbus. Low-level clouds do not have any altitude-related prefixes. However mid-level stratiform and stratocumuliform types are given the prefix alto- while high-level variants of these same two forms carry the prefix cirro-. Genus types with sufficient vertical extent to occupy more than one level do not carry any altitude related prefixes. They are classified formally as low- or mid-level depending on the altitude at which each initially forms, and are also more informally characterized as multi-level or vertical. Most of the ten genera derived by this method of classification can be subdivided into species and further subdivided into varieties. Very low stratiform clouds that extend down to the Earth's surface are given the common names fog and mist, but have no Latin names. 64909
Siberian Huskies at Retordica, Plateau de Retord, Cuvéry, Ain, France
For more than 25 years, an international dog sled race has been taking place in the wilderness of Plateau de Retord. Many mushers love this site to train their teams throughout the winter.
The sled dog racing is subdivided into several categories according to the number of dogs harnessed and in three subcategories according to the breed of dogs harnessed.
Indeed, the faster Siberian Husky compete in a separate category, the other three breeds : Alaskan Malamute, Samoyed and Greenland dog run in the same category, while the so-called "Nordic type" dogs participate in their own category.
In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body or similar space. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere, which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology. There are two methods of naming clouds in their respective layers of the homosphere, Latin and common. Genus types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adoption of Luke Howard's nomenclature that was formally proposed in 1802. It became the basis of a modern international system that divides clouds into five physical forms which can be further divided or classified into altitude levels to derive ten basic genera. The main representative cloud types for each of these forms are stratus, cirrus, stratocumulus, cumulus, and cumulonimbus. Low-level clouds do not have any altitude-related prefixes. However mid-level stratiform and stratocumuliform types are given the prefix alto- while high-level variants of these same two forms carry the prefix cirro-. Genus types with sufficient vertical extent to occupy more than one level do not carry any altitude related prefixes. They are classified formally as low- or mid-level depending on the altitude at which each initially forms, and are also more informally characterized as multi-level or vertical. Most of the ten genera derived by this method of classification can be subdivided into species and further subdivided into varieties. Very low stratiform clouds that extend down to the Earth's surface are given the common names fog and mist, but have no Latin names. R_8306
A team of 12 Siberian Huskies and the musher at Retordica, Plateau de Retord, Cuvéry, Ain, France
For more than 25 years, an international dog sled race has been taking place in the wilderness of Plateau de Retord. Many mushers love this site to train their teams throughout the winter.
The sled dog racing is subdivided into several categories according to the number of dogs harnessed and in three subcategories according to the breed of dogs harnessed.
Indeed, the faster Siberian Husky compete in a separate category, the other three breeds : Alaskan Malamute, Samoyed and Greenland dog run in the same category, while the so-called "Nordic type" dogs participate in their own category.
Absolutely no manipulation involved! This cloud which looked just like a porpoise was hovering near my brother's property in Orange, New South Wales.
In meteorology, a cloud is an aerosol comprising a visible mass of minute liquid droplets, frozen crystals, or particles suspended in the atmosphere above the surface of a planetary body. The droplets and crystals may be made of water or various chemicals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere (which includes the troposphere, stratosphere, and mesosphere). Nephology is the science of clouds which is undertaken in the cloud physics branch of meteorology.
There are two methods of naming clouds in their respective layers of the atmosphere; Latin and common. Cloud types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adaptation of Luke Howard's nomenclature. Formally proposed in 1802, it became the basis of a modern international system that divides clouds into five physical forms that appear in any or all of three altitude levels (formerly known as étages). These physical types, in approximate ascending order of convective activity, include stratiform sheets, cirriform wisps and patches, stratocumuliform layers (mainly structured as rolls, ripples, and patches), cumuliform heaps, and very large cumulonimbiform heaps that often show complex structure. The physical forms are divided by altitude level into ten basic genus-types. The Latin names for applicable high-level genera carry a cirro- prefix, and an alto- prefix is added to the names of the mid-level genus-types. Most of the genera can be subdivided into species and further subdivided into varieties.
Two cirriform clouds that form higher up in the stratosphere and mesosphere have common names for their main types. They are seen infrequently, mostly in the polar regions of Earth. Clouds have been observed in the atmospheres of other planets and moons in the Solar System and beyond. However, due to their different temperature characteristics, they are often composed of other substances such as methane, ammonia, and sulfuric acid as well as water.
Taken as a whole, homospheric clouds can be cross-classified by form and level to derive the ten tropospheric genera and the two additional major types above the troposphere. The cumulus genus includes three species that indicate vertical size. Clouds with sufficient vertical extent to occupy more than one altitude level are officially classified as low- or mid-level according to the altitude range at which each initially forms. However they are also more informally classified as multi-level or vertical.
For further information please visit en.wikipedia.org/wiki/Cloud
The Polar Adventure : Méaudre, Isere, France
This sport takes back ancestral traditions which allowed the Inuits to survive in the big Arctic deserts and represent the link with the nature.
The sled dog racing is subdivided into several categories according to the number of dogs harnessed and in three subcategories according to the breed of dogs harnessed.
Indeed, the faster Siberian Husky compete in a separate category, the other three breeds : Alaskan Malamute, Samoyed and Greenland dog run in the same category, while the so-called "Nordic type" dogs participate in their own category.
Reserva Natural Río Blanco, Manizales Colombia.
This strikingly plumaged antpitta is both easily identified and one of the most easily seen of an extremely wary and notoriously shy family of birds.
Chestnut-crowned Antpitta ranges from northern Venezuela south to central Peru, and is subdivided into seven subspecies, which mainly differ in the details of their head patterns. It has a broad altitudinal range, from 1200 to 3600 m, and is found in all manner of forest types, but especially favors borders, clearings, second growth, patches of bamboo, and other disturbed habitats.
Photo taken at Reserva Natural Río Blanco. Here travelers can walk by ecological trails. It has an area of 4,932 hectares of cloud forest and is between 2,150 meters and 3,700 meters above sea level.
neotropical.birds.cornell.edu/Species-Account/nb/species/...
The Galveston Silk Stocking local historic district was created in 1975, with 25th Street, or Rosenberg, as the core thoroughfare. The neighborhood is one of the most intact residential areas in the city from the late 19th and early 20th century. It is also a National Register Historic District. The name of the district refers to the wealth of the early residents – that they could afford to buy silk stockings. Silk Stocking was originally developed in the early 1870s as a mix of single-family houses, a small corner store, large vacant blocks and industrial sites. Until the 1890s, the core of the Silk Stocking District was occupied by the Texas Cotton Press. After the Texas Press went bankrupt and was demolished, the area was subdivided and the lots sold at auction in 1898
Flora is all the plant life present in a particular region or time, generally the naturally occurring (indigenous) native plants. Sometimes bacteria and fungi are also referred to as flora, as in the terms gut flora or skin flora.
The word "flora" comes from the Latin name of Flora, the goddess of plants, flowers, and fertility in Roman mythology. The technical term "flora" is then derived from a metonymy of this goddess at the end of the sixteenth century. It was first used in poetry to denote the natural vegetation of an area, but soon also assumed the meaning of a work cataloguing such vegetation. Moreover, "Flora" was used to refer to the flowers of an artificial garden in the seventeenth century.
Plants are grouped into floras based on region (floristic regions), period, special environment, or climate. Regions can be distinct habitats like mountain vs. flatland. Floras can mean plant life of a historic era as in fossil flora. Lastly, floras may be subdivided by special environments:
Native flora. The native and indigenous flora of an area.
Agricultural and horticultural flora (garden flora). The plants that are deliberately grown by humans.
Weed flora. Traditionally this classification was applied to plants regarded as undesirable, and studied in efforts to control or eradicate them. Today the designation is less often used as a classification of plant life, since it includes three different types of plants: weedy species, invasive species (that may or may not be weedy), and native and introduced non-weedy species that are agriculturally undesirable. Many native plants previously considered weeds have been shown to be beneficial or even necessary to various ecosystems. Source Wikipedia.
TD : 1/250 f/8 ISO 100 @28mm Pentax-M lens on hybrid Alpha 6000
Reserva Natural Río Blanco, Manizales Colombia.
Grallaria ruficapilla
(Chestnut-crowned Antpitta / Tororoi comprapán)
This strikingly plumaged antpitta is both easily identified and one of the most easily seen of an extremely wary and notoriously shy family of birds.
Chestnut-crowned Antpitta ranges from northern Venezuela south to central Peru, and is subdivided into seven subspecies, which mainly differ in the details of their head patterns. It has a broad altitudinal range, from 1200 to 3600 m, and is found in all manner of forest types, but especially favors borders, clearings, second growth, patches of bamboo, and other disturbed habitats.
Photo taken at Reserva Natural Río Blanco. Here travelers can walk by ecological trails. It has an area of 4,932 hectares of cloud forest and is between 2,150 meters and 3,700 meters above sea level.
neotropical.birds.cornell.edu/Species-Account/nb/species/...
In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body or similar space. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere, which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology. There are two methods of naming clouds in their respective layers of the homosphere, Latin and common. Genus types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adoption of Luke Howard's nomenclature that was formally proposed in 1802. It became the basis of a modern international system that divides clouds into five physical forms which can be further divided or classified into altitude levels to derive ten basic genera. The main representative cloud types for each of these forms are stratus, cirrus, stratocumulus, cumulus, and cumulonimbus. Low-level clouds do not have any altitude-related prefixes. However mid-level stratiform and stratocumuliform types are given the prefix alto- while high-level variants of these same two forms carry the prefix cirro-. Genus types with sufficient vertical extent to occupy more than one level do not carry any altitude related prefixes. They are classified formally as low- or mid-level depending on the altitude at which each initially forms, and are also more informally characterized as multi-level or vertical. Most of the ten genera derived by this method of classification can be subdivided into species and further subdivided into varieties. Very low stratiform clouds that extend down to the Earth's surface are given the common names fog and mist, but have no Latin names.
Two things contribute to the moon being visible in daylight. First, it is bright enough that its light penetrates the scattered blue light of the sky. If you're looking at exactly the right spot with a telescope, you can also see the planets Mercury, Venus, and Jupiter in daylight, plus a few of the brightest stars (though few casual observers can actually pull this off). Secondly, the moon must be high enough in the sky to be visible. Because of the Earth's rotation, the moon is above the horizon roughly 12 hours out of every 24. Since those 12 hours almost never coincide with the roughly 12 hours of daylight in every 24 hours, the possible window for observing the moon in daylight averages about 6 hours a day. The moon is visible in daylight nearly every day, the exceptions being close to new moon, when the moon is too close to the sun to be visible, and close to full moon when it is only visible at night. The best times in the month to see the moon in daylight are close to first and last quarter, when the moon is 90 degrees away from the sun in the sky. R_6972
The speckled wood (Pararge aegeria) is a of woodland areas throughout much of the Palearctic ecozone.[1] The species is subdivided into multiple subspecies, including Pararge aegeria aegeria,[1] Pararge aegeria tircis, Pararge aegeria oblita, and Pararge aegeria insula.[2] The color of this butterfly varies between subspecies. The existence of these subspecies is due to variation in morphology down a gradient corresponding to a geographic cline.[3] The background of the wings ranges from brown to orange, and the spots are either pale yellow, white, cream, or a tawny orange. The speckled wood feeds on a variety of grass species.[2] The males of this species exhibit two types of mate locating behaviors: territorial defense and patrolling.[4] The proportion of males exhibiting these two strategies changes based on ecological conditions.[4][5] The monandrous female must choose which type of male can help her reproduce successfully. Her decision is heavily influenced by environmental conditions
Reserva Natural Río Blanco, Manizales Colombia.
This strikingly plumaged antpitta is both easily identified and one of the most easily seen of an extremely wary and notoriously shy family of birds.
Chestnut-crowned Antpitta ranges from northern Venezuela south to central Peru, and is subdivided into seven subspecies, which mainly differ in the details of their head patterns. It has a broad altitudinal range, from 1200 to 3600 m, and is found in all manner of forest types, but especially favors borders, clearings, second growth, patches of bamboo, and other disturbed habitats.
Photo taken at Reserva Natural Río Blanco. Here travelers can walk by ecological trails. It has an area of 4,932 hectares of cloud forest and is between 2,150 meters and 3,700 meters above sea level.
neotropical.birds.cornell.edu/Species-Account/nb/species/...
Back to the Kleinwalsertal, with a photo of an old farm, that is now a protected monument. It is a "Walserhaus", a house that was built by the Walser, the immigrants who came from Wallis, Switzerland. Houses like this can be 400 or even 500 years old. Original elements have survived, like the roof that protrudes and the way the glass of the windows is subdivided - as you can see in this photo.
I'm interested in old architecture and love wooden buildings. This house attracted my attention at the start of a walk into the Gemsteltal. I also think the abundance of flowers at the windows is fantastic!
In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body or similar space. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere, which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology. There are two methods of naming clouds in their respective layers of the homosphere, Latin and common. Genus types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adoption of Luke Howard's nomenclature that was formally proposed in 1802. It became the basis of a modern international system that divides clouds into five physical forms which can be further divided or classified into altitude levels to derive ten basic genera. The main representative cloud types for each of these forms are stratus, cirrus, stratocumulus, cumulus, and cumulonimbus. Low-level clouds do not have any altitude-related prefixes. However mid-level stratiform and stratocumuliform types are given the prefix alto- while high-level variants of these same two forms carry the prefix cirro-. Genus types with sufficient vertical extent to occupy more than one level do not carry any altitude related prefixes. They are classified formally as low- or mid-level depending on the altitude at which each initially forms, and are also more informally characterized as multi-level or vertical. Most of the ten genera derived by this method of classification can be subdivided into species and further subdivided into varieties. Very low stratiform clouds that extend down to the Earth's surface are given the common names fog and mist, but have no Latin names. R_6940
Volcanic activity after the eruption of the ignimbrite has been subdivided into the older andesitic Purico group and the younger Chascon group.
The first includes Cerro Negro, Cerro Purico, Putas and Cerro Toco which assume the structure of polygenetic volcanoes, while the latter is taken to include Aspero, El Cerillo/Chajnantor and El Chascon which are lava dome-lava flow structures. The Chascon group of domes is also the only one which contains mafic xenoliths.
Burano is an island in the Venetian Lagoon, northern Italy, near Torcello at the northern end of the Lagoon, known for its lace work and brightly coloured homes. The primary economy is tourism.
Burano is 7 kilometres (4 miles) from Venice, a 40-minute trip from St. Mark's Square by a Venetian water bus, vaporetto.
The island is linked to Mazzorbo by a bridge.The current population of Burano is about 2,800. Originally, there were five islands and a fourth canal that was filled to become via e piazza Baldassare Galuppi, joining the former islands of San Martino Destra and San Martino Sinistra.
Burano has historically been subdivided into five sestieri, much like Venice. They correspond to the five original islands. The sixth sestiere is neighbouring Mazzorbo.
Burano is also known for its small, brightly painted houses, which are popular with artists. The colours of the houses follow a specific system, originating from the golden age of its development. If someone wishes to paint their home, one must send a request to the government, who will respond by making notice of the certain colours permitted for that lot.
Other attractions include the Church of San Martino, with a leaning campanile and a painting by Giambattista Tiepolo (Crucifixion, 1727), the Oratorio di Santa Barbara and the Museum and School of Lacemaking.
Taken in January 2004, the end of an era with Crown Garage closing. It was subdivided into two shops.
Travel Photography by KeefH Web Designs
shot by KHWD, a fabulous stretch of beach inhabited by Rover, the security balloon / zorb
Rover is a plot device from the 1967 British television programme The Prisoner, and was a crucial tool used to keep 'prisoners' from escaping the Village. It was depicted as a floating white balloon that could coerce, and, if necessary, incapacitate or kill recalcitrant inhabitants of the Village. It also had the ability to subdivide. Several aspects of the Rover device were left unexplained and to the imagination of the viewer.
The name "Rover" was only used once in the entire series (in the episode "The Schizoid Man"). The novel The Prisoner: Number Two by David McDaniel, based upon the series, uses the name Guardian.
Naples Botanical Gardens
60 Acre Wildlife Reserve
Naples, FL
Click twice on image for best view.
The anhinga (Anhinga anhinga), sometimes called snakebird, darter, American darter, or water turkey, is a water bird of the warmer parts of the Americas. The word anhinga comes from the Brazilian Tupi language and means devil bird or snake bird. The origin of the name snakebird is apparent when swimming: only the colored neck appears above water so the bird looks like a snake ready to strike. They do not have external nares (nostrils) and breathe solely through their epiglottis.
The anhinga is placed in the darter family, Anhingidae, and is closely related to Indian (Anhinga melanogaster), African (Anhinga rufa), and Australian (Anhinga novaehollandiae) darters. Like other darters, the anhinga hunts by spearing fish and other small prey using its sharp, slender beak.
Anhinga species are found all over the world in warm shallow waters. The American anhinga has been subdivided into two subspecies, A. a. anhinga and A. a. leucogaster, based on their location. A. a. leucogaster can be found in the southern United States, Mexico, Cuba, and Grenada. A fossil species Anhinga walterbolesi has been described from the Late Oligocene to Early Miocene of Australia.
Only birds that live in the extreme north and south of their range migrate and do so based on temperature and available sunlight. Anhingas will migrate towards the equator during winter but this range is "determined by the amount of sunshine to warm the chilled birds". Although not in their usual range, anhingas have been found as far north as the states of Pennsylvania and Wisconsin in the United States. Wikipedia
Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast, that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico.
Canada officially defines the Rocky Mountains system as the mountain chains east of the Rocky Mountain Trench extending from the Liard River valley in northern British Columbia to the Albuquerque Basin in New Mexico, not including the Mackenzie, Richardson and British Mountains/Brooks Range in Yukon and Alaska (which are all included as the "Arctic Rockies" in the United States' definition of the Rocky Mountains system). The Canadian Rockies, being the northern segment of this chain, is thus defined as comprising the central-eastern section of the North American Cordillera, between the Prairies of Alberta and the Liard Plain of northeastern British Columbia to the east and the Interior Mountains/Plateau and Columbia Mountains to the west. It is divided into the Northern Rockies (which is further subdivided into the Muskwa and Hart Ranges) and Continental Ranges, separated by the McGregor River valley, the McGregor Pass and the Kakwa River valley.
The southern end of the Canadian Rockies extends into the U.S. state of Montana at various sites such as the Wilson Range, Upper Waterton Lake, Boundary Creek, Cameron Lake, Forum Peak, Long Knife Peak, North Fork Flathead River and Frozen Lake. In geographic terms, the boundary is at the Canada–United States border on 49th parallel north, but in geological terms it might be considered to be at Marias Pass in northern Montana.
The Canadian Rockies have numerous high peaks and ranges, such as Mount Robson (3,954 metres; 12,972 feet) and Mount Columbia (3,747 m; 12,293 ft). The Canadian Rockies are composed of shale and limestone. Much of the range is protected by national and provincial parks, several of which collectively comprise a World Heritage Site.
I subdivided all the hostas last year except this Big Daddy, and they may not bloom yet this season. So Big Daddy will likely be the only blooming hosta for 2020.
The brown corn bolt (Libellula fulva) is a species of dragonfly from the family of corn bolts (Libellulidae), subdivided real dragonflies (Anisoptera). It is a striking orange or blue appearance that is quite rare in the Netherlands.
De bruine korenbout (Libellula fulva) is een libellensoort uit de familie van de korenbouten(Libellulidae), onderorde echte libellen (Anisoptera). Het is een opvallende oranje of blauwe verschijning die in Nederland vrij zeldzaam is.
An old Chinese ruler with units of measurement called ‘cun’. Ten ‘cun’ equals one ‘chi’. The ‘cun’ is in turn subdivided into 10 units, and shown here. A ‘cun’ is equal to about 3.3cm. The width of the flower ( Tulbaghia violacea, aka Society Garlic) is around 4/10 of a ‘cun’ (ie approx 1.3 cm or 1/2”). See comments for a larger view
98/100 flowers
Burano is an island in the Venetian Lagoon, northern Italy, near Torcello at the northern end of the Lagoon, known for its lace work and brightly coloured homes. The primary economy is tourism.
Burano is 7 kilometres (4 miles) from Venice, a 40-minute trip from St. Mark's Square by a Venetian water bus, vaporetto.
The island is linked to Mazzorbo by a bridge.The current population of Burano is about 2,800. Originally, there were five islands and a fourth canal that was filled to become via e piazza Baldassare Galuppi, joining the former islands of San Martino Destra and San Martino Sinistra.
Burano has historically been subdivided into five sestieri, much like Venice. They correspond to the five original islands. The sixth sestiere is neighbouring Mazzorbo.
Burano is also known for its small, brightly painted houses, which are popular with artists. The colours of the houses follow a specific system, originating from the golden age of its development. If someone wishes to paint their home, one must send a request to the government, who will respond by making notice of the certain colours permitted for that lot.
More Leica photography at The Leica Society www.theleicasociety.org.uk/
Palgon དཔལ་མགོན། county
Palgon county in the hinterland of Lake Namtso Chukmo. Until recently Palgon was one of largest of the Jangtang counties (being Shentsa the largest), extending from the present-day Xinjiang and Qinghai provincial borders in the north to the Yarlung Tsangpo ཡར་ཀླུངས་གཙང་པོ་ (Brahmaputra) watershed in the south. As such the county was larger than the United Kingdom! But now it has been subdivided into Tsonyi county and Palgon proper, governed from Naktsang. The county capital is located at Namru. Area: 99.112 sq km. www.footprinttravelguides.com/c/2848/tibet/&Action=pr...
Eilean Donan Castle went through several phases of development from the earliest fortifications of the 13th century through to its destruction in 1719, and the subsequent reconstruction in the 20th century. The first phase comprised a curtain wall enclosing much of the island with a tower house added in the 14th century. In the 14th or 15th century the outer wall was abandoned and a smaller enclosure built around the tower house. More development within this courtyard took place in the 16th century, as well as the addition of defences on the eastern side. The castle was almost totally destroyed in 1719, after which almost 200 years passed before reconstruction began. Although some archaeological evidence has been recovered from the island, much material was lost during the reconstruction works making it difficult to build a clear picture of the early castle. Very little historical evidence survives.
The castell of Ylen Donen is composed of a strong and fair dungeon upon a rock, with another tower compasd with a fair barmkin wall, with orchards and trees, al within ane yland of the lenth of twa pair of butts almost round. It is sayd of old that castel consisted of seven tours.
The only drawing of the castle prior to its destruction was made in 1714 by Lewis Petit (c. 1665–1720), a military engineer with the Board of Ordnance who came to Scotland in 1714 to survey Fort William and other defences in the area. Among the drawings he produced are a plan and elevation of Eilean Donan, which clearly show that the castle was largely derelict by this time, with only a building at the southeast corner being roofed. In the 13th century, a curtain wall or wall of enceinte was constructed around the island, enclosing most of the area above the high tide line. Scant remains of these walls can be traced on the ground, running around the northern end of the island. The eastern and southern segments of this wall are largely obscured by later development, although the enclosure is assumed to have contained an area of around 3,000 square metres (32,000 square feet). At the northern point of the wall the foundations of a large tower survive, measuring around 12 by 13 metres (39 by 43 ft) and the remains of foundations suggest further towers at the north-east and southwest corners of the enclosure. The enclosure was accessed via a sea-gate in the north-west curtain wall, where a small beach would have allowed boats to be drawn up. Another beach to the southwest may have formed a second access. Archaeological excavations in 2008 and 2009 confirmed the presence of these walls, and also found evidence that metalworking was taking place in the northern part of the castle. A tower house or keep was built against the curtain wall at the high point of the island, probably in the 14th century. The tower measured 16.5 by 12.4 m (54 ft 2 in by 40 ft 8 in), with walls 3 m (9 ft 10 in) thick. The vaulted ground floor was originally divided in two, with a stair in the north wall giving access to the first-floor hall. Above this were probably another two storeys, including a garret. The tower, according to Petit's later drawing, was topped by crowstep gables, and surrounded by a walkway and bartizans (small turrets) at the corners.
At an unknown period, probably in the later 14th century or early 15th century, the outer wall was abandoned in favour of a smaller defensive enclosure, around 25 m (82 ft) square. The entrance to this smaller courtyard was from the east. The reasons for this change are unclear, though it is suggested that the smaller area would have been easier to defend. During the 16th century, two buildings were added to the southern periphery of the enclosure. A small house was constructed within the southeast angle of the wall, with a circular stair-tower on its northern side giving access to the walkway along the eastern curtain wall. Located just inside the gate, this is likely to have served as a house for the castle's constable or keeper, and is the only building shown with a roof on Petit's survey. At the southwest corner of the enclosure, an L-plan block was put up, possibly as late as the early 17th century. The southern part is sited outside the line of the inner curtain wall, with a northern wing, which may have been a slightly later addition, inside the wall.
A mural chamber within the keep
In the later 16th century, the castle was extended eastward to create a bastion or "hornwork", providing a more securely defended entrance. The hornwork comprises a pair of walls enclosing a triangular courtyard, linking the east wall of the castle with an irregular hexagonal (or heptagonal) structure. This structure, 11.5 m (37 ft 9 in) across, contains a well at its lowest level, 5 m (16 ft) across and 10 m (33 ft) deep. This led MacGibbon and Ross to describe the structure as a water tower or cistern. However, the presence of a door on its eastern side is shown in 19th century photographs, indicating that it was built as the main entrance to the castle. The water-filled interior would have been crossed by a removable bridge, presenting an obstacle to attackers. From the bridge, access to the castle would have been up a flight of steps, into the triangular courtyard, and through the gate in the east curtain wall. It is possible that the hexagonal bastion was roofed to serve as an artillery position. Dredging of the reservoir in 1893 recovered two brass guns, referred to as "double hagbuts", and measuring around 1 m (3 ft) long with a bore of around 25 millimetres (1 in). Also recovered was a yett, an iron gate, probably installed in the east door to the bastion, but now on display inside the castle. At some point in the 17th century, this elaborate access was abandoned and a more convenient entrance opened in the south wall of the hornwork. By 1714, Lewis Petit's drawing clearly shows that the castle was largely derelict, with only the house at the southeast corner being roofed. Four years later, it was completely demolished, and, by 1912, very little of the castle was still standing.
The present castle buildings are entirely the result of 20th-century reconstruction by Gilstrap-Macrae, who commissioned Edinburgh architect George Mackie Watson to draw up the plans. Although the rebuilding followed the extant ground plan, the details of the present castle differ from its original appearance. The survey drawings by Lewis Petit were not rediscovered until the restoration was almost complete, and the restorers therefore were forced to rely on less accurate interpretations such as the work of MacGibbon and Ross, who attempted a plan of the remains in the late 19th century. The clerk of works, Farquhar Macrae, is said to have based the reconstruction on a dream in which he saw the restored Eilean Donan.Rather than a genuinely medieval castle, Eilean Donan is described as "a romantic reincarnation in the tradition of early 20th-century castle revivals." John Gifford, analysing the building against the Petit survey, notes a "fussy elaboration of what was probably plain originally, and an omission of decoration where it once existed", and describes the interior as "a rubbly Edwardian stage-set for life in the Middle Ages".
The castle is today entered from the south, via a modern portal complete with a portcullis. Above the door is a Gaelic inscription which in translation reads: "As long as there is a Macrae inside, there will never be a Fraser outside", referring to a bond of kinship between the two clans, and a similar inscription which once adorned the Fraser's home at Beaufort Castle. Above this is carved the coat of arms of John Macrae-Gilstrap. The portal gives access to the courtyard, the level of which has been lowered exposing the bedrock around the tower house. The present buildings at the southeast of the castle reflect the form of the earlier structures, including the circular stair tower, but are larger in extent. To the southwest only the southern portion of the L-shaped block was reconstructed, as a plain three-storey house, while in place of the northern wing is an open platform giving views over the loch. A small tower occupies the north-west angle. The keep itself follows the original dimensions, though the formerly subdivided ground floor is now a single room: the tunnel-vaulted Billeting Hall. Above on the first floor is the Banqueting Hall with an oak ceiling, and decorated with coats of arms and 15th-century style fireplace. The main ceiling beams in the Banqueting Hall are of Douglas Fir and were shipped from British Columbia, Canada as a gift from the Macraes of Canada. Small mural chambers within the walls are accessed from each hall.