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day 3
this wall is built between falls road (catholic neighbourhood) and shankill road (protestand neighbourhood). it's about 5 meters high.
there are dozens of these border barriers in northern ireland, that separate irish nationalist and unionist neighbourhoods. they have been built at urban interface areas in belfast, derry, portadown and other towns. the stated purpose of the walls is to minimise inter-communal violence between catholics, most of whom are nationalists who self-identify as irish, and protestants, most of whom are unionists who self-identify as british.
in a great exhibition of understatement, these walls are named "peace lines"
241/365
This border around my mother's house separates the bushes and trees that line the outside of the house from the front lawn. It started with a cutting from a neighbor over 40 years and quickly grew into a thick, lush border that needs little care. In fact, it needs to be controlled and cut back or it will take over. Until I looked it up, my mother wasn't even sure what it was.
"Pachysandra terminalis, the Japanese pachysandra, carpet box or Japanese spurge, is a species of flowering plant in the boxwood family Buxaceae, native to Japan, Korea, and China and introduced to eastern North America. When growing in a spreading mass of many plants, a dense cover is formed." -- en.wikipedia.org
It seems that almost every plant or flower I admire here in the NYC environs turns out to be native to eastern Asia. One example of how humans have altered the environment.
One photo a day. (187/366) Bayside, Queens, NYC -- July 5, 2020
en.wikipedia.org/wiki/Mediterranean_Sea
The Mediterranean Sea is a sea connected to the Atlantic Ocean surrounded by the Mediterranean region and almost completely enclosed by land: on the north by Europe and Anatolia, on the south by North Africa, and on the east by the Levant. The sea is sometimes considered a part of the Atlantic Ocean, although it is usually identified as a completely separate body of water.
The name Mediterranean is derived from the Latin mediterraneus, meaning "inland" or "in the middle of the land" (from medius, "middle" and terra, "land"). It covers an approximate area of 2.5 million km² (965,000 sq mi), but its connection to the Atlantic (the Strait of Gibraltar) is only 14 km (8.7 mi) wide. In oceanography, it is sometimes called the Eurafrican Mediterranean Sea or the European Mediterranean Sea to distinguish it from mediterranean seas elsewhere.[3][4]
The Mediterranean Sea has an average depth of 1,500 m (4,900 ft) and the deepest recorded point is 5,267 m (17,280 ft) in the Calypso Deep in the Ionian Sea.
It was an important route for merchants and travellers of ancient times that allowed for trade and cultural exchange between emergent peoples of the region. The history of the Mediterranean region is crucial to understanding the origins and development of many modern societies.
Name
The term Mediterranean derives from the Latin word mediterraneus, meaning "in the middle of earth" or "between lands" (medi-; adj. medius, -um -a "middle, between" + terra f., "land, earth"): as it is between the continents of Africa, Asia and Europe. The Greek name Mesogeios (Μεσόγειος), is similarly from μέσο, "middle" + γη, "land, earth").[5]
The Mediterranean Sea has historically had several names. For example the Romans commonly called it Mare Nostrum (Latin, "Our Sea"), and occasionally Mare Internum (Sallust, Jug. 17).
In the Bible, it was primarily known as הים הגדול (HaYam HaGadol), the "Great Sea", (Num. 34:6,7; Josh. 1:4, 9:1, 15:47; Ezek. 47:10,15,20), or simply "The Sea" (1 Kings 5:9; comp. 1 Macc. 14:34, 15:11); however, it has also been called the "Hinder Sea", due to its location on the west coast of the Holy Land, and therefore behind a person facing the east, sometimes translated as "Western Sea", (Deut. 11:24; Joel 2:20). Another name was the "Sea of the Philistines" (Exod. 23:31), from the people occupying a large portion of its shores near the Israelites.
In Modern Hebrew, it has been called HaYam HaTikhon (הַיָּם הַתִּיכוֹן), "the Middle Sea", reflecting the Sea's name in ancient Greek (Mesogeios), Latin (Mare internum) and modern languages in both Europe and the Middle East (Mediterranean, etc.). Similarly, in Modern Arabic, it is known as al-Baḥr [al-Abyaḍ] al-Mutawassiṭ (البحر [الأبيض] المتوسط), "the [White] Medium Sea", while in Islamic and older Arabic literature, it was referenced as Baḥr al-Rūm (بحر الروم), or "the Roman/Byzantine Sea." In Turkish, it is known as Akdeniz,[6] "the White Sea" since among Turks the white color (ak) represents the west.
History
Several ancient civilizations were located around its shores; thus it has had a major influence on those cultures. It provided routes for trade, colonization and war, and provided food (by fishing and the gathering of other seafood) for numerous communities throughout the ages.[7]
The sharing of similar climate, geology and access to a common sea led to numerous historical and cultural connections between the ancient and modern societies around the Mediterranean.
Two of the most notable Mediterranean civilizations in classical antiquity were the Greek city states and the Phoenicians. When[citation needed] Augustus founded the Roman Empire, the Mediterranean Sea began to be called Mare Nostrum (literally:"Our Sea") by the Romans.
Darius I of Persia, who conquered Ancient Egypt, built a canal linking the Mediterranean to the Red Sea. Darius's canal was wide enough for two triremes to pass each other with oars extended, and required four days to traverse.[8]
The western Roman empire collapsed around AD 476. Temporarily the east was again dominant as the Byzantine Empire formed from the eastern half of the Roman empire. Another power soon arose in the east: Islam. At its greatest extent, the Arab Empire controlled 75% of the Mediterranean region.
Europe was reviving, however, as more organized and centralized states began to form in the later Middle Ages after the Renaissance of the 12th century.
Ottoman power continued to grow, and in 1453, the Byzantine Empire was extinguished with the Conquest of Constantinople. Ottomans gained control of much of the sea in the 16th century and maintained naval bases in southern France, Algeria and Tunisia. Barbarossa, the famous Ottoman captain is a symbol of this domination with the victory of the Battle of Preveza. The Battle of Djerba marked the apex of Ottoman naval domination in the Mediterranean. However, as naval prowess of the European powers grew, they confronted Ottoman expansion in the region when the Battle of Lepanto checked the power of the Ottoman Navy. This was the last naval battle to be fought primarily between galleys.
The Barbary pirates of North Africa preyed on Christian shipping in the western Mediterranean Sea.[9] According to Robert Davis, from the 16th to 19th century, pirates captured 1 million to 1.25 million Europeans as slaves.[10]
The development of oceanic shipping began to affect the entire Mediterranean. Once, all trade from the east had passed through the region, but now the circumnavigation of Africa allowed spices and other goods to be imported through the Atlantic ports of western Europe.[11][12][13] The Malta president described the Mediterranean sea as a "cemetery" due to the large amounts of migrants who drown there.
Geography
With its highly indented coastline and large number of islands, Greece has the longest Mediterranean coastline.
The Mediterranean Sea is connected to the Atlantic Ocean by the Strait of Gibraltar in the west and to the Sea of Marmara and the Black Sea, by the Dardanelles and the Bosporus respectively, in the east. The Sea of Marmara is often considered a part of the Mediterranean Sea, whereas the Black Sea is generally not. The 163 km (101 mi) long man-made Suez Canal in the southeast connects the Mediterranean Sea to the Red Sea.
Large islands in the Mediterranean include Cyprus, Crete, Euboea, Rhodes, Lesbos, Chios, Kefalonia, Corfu, Limnos, Samos, Naxos and Andros in the eastern Mediterranean; Sardinia, Corsica, Sicily, Cres, Krk, Brač, Hvar, Pag, Korčula and Malta in the central Mediterranean; and Ibiza, Majorca and Minorca (the Balearic Islands) in the western Mediterranean.
The typical Mediterranean climate has hot, dry summers and mild, rainy winters. Crops of the region include olives, grapes, oranges, tangerines, and cork.
Extent
The International Hydrographic Organization defines the limits of the Mediterranean Sea as follows:[15]
Stretching from the Strait of Gibraltar in the West to the entrances to the Dardanelles and the Suez Canal in the East, the Mediterranean Sea is bounded by the coasts of Europe, Africa and Asia, and is divided into two deep basins:
Western Basin:
On the west: A line joining the extremities of Cape Trafalgar (Spain) and Cape Spartel (Africa).
On the northeast: The West Coast of Italy. In the Strait of Messina a line joining the North extreme of Cape Paci (15°42'E) with Cape Peloro, the East extreme of the Island of Sicily. The North Coast of Sicily.
On the east: A line joining Cape Lilibeo the Western point of Sicily (37°47′N 12°22′E), through the Adventure Bank to Cape Bon (Tunisia).
Eastern Basin:
On the west: The Northeastern and Eastern limits of the Western Basin.
On the northeast: A line joining Kum Kale (26°11'E) and Cape Helles, the Western entrance to the Dardanelles.
On the southeast: The entrance to the Suez Canal.
On the east: The coasts of Syria, Israel, Lebanon, and Gaza Strip.
Oceanography
Being nearly landlocked affects conditions in the Mediterranean Sea: for instance, tides are very limited as a result of the narrow connection with the Atlantic Ocean. The Mediterranean is characterized and immediately recognised by its deep blue colour.
Evaporation greatly exceeds precipitation and river runoff in the Mediterranean, a fact that is central to the water circulation within the basin.[16] Evaporation is especially high in its eastern half, causing the water level to decrease and salinity to increase eastward.[17] This pressure gradient pushes relatively cool, low-salinity water from the Atlantic across the basin; it warms and becomes saltier as it travels east, then sinks in the region of the Levant and circulates westward, to spill over the Strait of Gibraltar.[18] Thus, seawater flow is eastward in the Strait's surface waters, and westward below; once in the Atlantic, this chemically distinct Mediterranean Intermediate Water can persist thousands of kilometres away from its source.
Coastal countries
Twenty-two countries have a coastline on the Mediterranean Sea. They are:
Northern shore (from west to east): Spain, France, Monaco, Italy, Slovenia, Croatia,
Bosnia and Herzegovina, Montenegro, Albania, Greece and Turkey.
Eastern shore (from north to south): Syria, Lebanon, Israel, Flag of Palestine.svg Palestine (limited recognition).
Southern shore (from west to east): Morocco, Algeria, Tunisia, Libya, Egypt.
Island nations: Malta, Cyprus, Flag of the Turkish Republic of Northern Cyprus.svg Northern Cyprus (limited recognition).
Several other territories also border the Mediterranean Sea (from west to east): The British overseas territory of Gibraltar, the Spanish autonomous cities of Ceuta and Melilla and nearby islands, and the Sovereign Base Areas on Cyprus
Major cities (municipalities) with populations larger than 200,000 people bordering the Mediterranean Sea are:
CountryCities
AlbaniaDurrës
AlgeriaAlgiers, Annaba, Oran
CroatiaSplit, Rijeka
EgyptAlexandria, Port Said
FranceMarseille, Nice
GreeceAthens, Patras, Thessaloniki
IsraelAshdod, Haifa, Tel Aviv
ItalyBari, Catania, Genoa, Messina, Naples, Palermo, Rome, Taranto, Trieste, Venice
LebanonBeirut, Tripoli
LibyaBenghazi, Khoms, Misrata, Tripoli, Zawiya, Zliten
MoroccoTétouan, Tangier
SpainAlicante, Badalona, Barcelona, Cartagena, Málaga, Palma, Valencia
State of PalestineGaza City
SyriaLatakia
TunisiaBizerte, Sfax, Tunis
TurkeyAntalya, İskenderun, İzmir, Mersin
Subdivisions
According to the International Hydrographic Organization (IHO), the Mediterranean Sea is subdivided into a number of smaller waterbodies, each with their own designation (from west to east):[15]
the Strait of Gibraltar;
the Alboran Sea, between Spain and Morocco;
the Balearic Sea, between mainland Spain and its Balearic Islands;
the Ligurian Sea between Corsica and Liguria (Italy);
the Tyrrhenian Sea enclosed by Sardinia, Italian peninsula and Sicily;
the Ionian Sea between Italy, Albania and Greece;
the Adriatic Sea between Italy, Slovenia, Croatia, Bosnia and Herzegovina, Montenegro and Albania;
the Aegean Sea between Greece and Turkey.
Other seas
Although not recognised by the IHO treaties, there are some other seas whose names have been in common use from the ancient times, or in the present:
the Sea of Sardinia, between Sardinia and Balearic Islands, as a part of the Balearic Sea
the Sea of Sicily between Sicily and Tunisia,
the Libyan Sea between Libya and Crete,
In the Aegean Sea,
the Thracian Sea in its north,
the Myrtoan Sea between the Cyclades and the Peloponnese,
the Sea of Crete north of Crete,
the Icarian Sea between Kos and Chios
the Cilician Sea between Turkey and Cyprus
the Levantine Sea at the eastern end of the Mediterranean
Other features
Many of these smaller seas feature in local myth and folklore and derive their names from these associations. In addition to the seas, a number of gulfs and straits are also recognised:
the Saint George Bay in Beirut, Lebanon
the Ras Ibn Hani cape in Latakia, Syria
the Ras al-Bassit cape in northern Syria.
the Minet el-Beida ("White Harbour") bay near ancient Ugarit, Syria
the Strait of Gibraltar, connects the Atlantic Ocean to the Mediterranean Sea and separates Spain from Morocco
the Bay of Gibraltar, at the southern end of the Iberian Peninsula
the Gulf of Corinth, an enclosed sea between the Ionian Sea and the Corinth Canal
the Pagasetic Gulf, the gulf of Volos, south of the Thermaic Gulf, formed by the Mount Pelion peninsula
the Saronic Gulf, the gulf of Athens, between the Corinth Canal and the Mirtoan Sea
the Thermaic Gulf, the gulf of Thessaloniki, located in the northern Greek region of Macedonia
the Kvarner Gulf, Croatia
the Gulf of Lion, south of France
the Gulf of Valencia, east of Spain
the Strait of Messina, between Sicily and the toe of Italy
the Gulf of Genoa, northwestern Italy
the Gulf of Venice, northeastern Italy
the Gulf of Trieste, northeastern Italy
the Gulf of Taranto, southern Italy
The Adriatic Sea contains over 1200 islands and islets.
the Gulf of Salerno, southwestern Italy
the Gulf of Gaeta, southwestern Italy
the Gulf of Squillace, southern Italy
the Strait of Otranto, between Italy and Albania
the Gulf of Haifa, northern Israel
the Gulf of Sidra, between Tripolitania (western Libya) and Cyrenaica (eastern Libya)
the Strait of Sicily, between Sicily and Tunisia
the Corsica Channel, between Corsica and Italy
the Strait of Bonifacio, between Sardinia and Corsica
the Gulf of İskenderun, between İskenderun and Adana (Turkey)
the Gulf of Antalya, between west and east shores of Antalya (Turkey)
the Bay of Kotor, in south-western Montenegro and south-eastern Croatia
the Malta Channel, between Sicily and Malta
the Gozo Channel, between Malta Island and Gozo
Sea temperature
Mean sea temperature (°C)
JanFebMarAprMayJunJulAugSepOctNovDecØ/Year
Marseille[21]13131314161821222118161416.6
Venice[22]11101113182225262320161417.4
Barcelona[23]13131314172023252320171517.8
Valencia[24]14131415172124262421181518.5
Málaga[25]16151516172022232220181618.3
Gibraltar[26]16151616172022222220181718.4
Naples[27]15141415182225272522191619.3
Athens[28]16151516182124242421191819.3
Heraklion[29]16151516192224252422201819.7
Malta[30]16161516182124262523211819.9
Larnaca[31]18171718202426272725221921.7
Limassol[32]18171718202426272725221921.7
Antalya17171718212427282725221921.8
Alexandria[33]18171718202325262625222021.4
Tel Aviv[34]18171718212426282726232022.1
Geology
The geologic history of the Mediterranean is complex. It was involved in the tectonic break-up and then collision of the African and Eurasian plates. The Messinian Salinity Crisis occurred in the late Miocene (12 million years ago to 5 million years ago) when the Mediterranean dried up. Geologically the Mediterranean is underlain by oceanic crust.
The Mediterranean Sea has an average depth of 1,500 m (4,900 ft) and the deepest recorded point is 5,267 m (17,280 ft) in the Calypso Deep in the Ionian Sea. The coastline extends for 46,000 km (29,000 mi). A shallow submarine ridge (the Strait of Sicily) between the island of Sicily and the coast of Tunisia divides the sea in two main subregions (which in turn are divided into subdivisions), the Western Mediterranean and the Eastern Mediterranean. The Western Mediterranean covers an area of about 0.85 million km² (0.33 million mi²) and the Eastern Mediterranean about 1.65 million km² (0.64 million mi²). A characteristic of the Mediterranean Sea are submarine karst springs or vruljas, which mainly occur in shallow waters[35] and may also be thermal.
Tectonic evolution
The geodynamic evolution of the Mediterranean Sea was provided by the convergence of European and African plates and several smaller microplates. This process was driven by the differential seafloor spreading along the Mid-Atlantic Ridge, which led to the closure of the Tethys Ocean and eventually to the Alpine orogenesis. However, the Mediterranean also hosts wide extensional basins and migrating tectonic arcs, in response to its land-locked configuration.
According to a report published by Nature in 2009, some scientists think that the Mediterranean Sea was mostly filled during a time period of less than two years, in a major flood (the Zanclean flood) that happened approximately 5.33 million years ago, in which water poured in from the Atlantic Ocean and through the Strait of Gibraltar, at a rate three times the current flow of the Amazon River.[37] However, the sea basins had been filled for many millions of years before the prior closure of the Strait of Gibraltar.
Eastern Mediterranean
In middle Miocene times, the collision between the Arabian microplate and Eurasia led to the separation between the Tethys and the Indian oceans. This process resulted in profound changes in the oceanic circulation patterns, which shifted global climates towards colder conditions. The Hellenic arc, which has a land-locked configuration, underwent a widespread extension for the last 20 Ma due to a slab roll-back process. In addition, the Hellenic Arc experienced a rapid rotation phase during the Pleistocene, with a counterclockwise component in its eastern portion and a clockwise trend in the western segment.
Central Mediterranean
The opening of small oceanic basins of the central Mediterranean follows a trench migration and back-arc opening process that occurred during the last 30 Myr. This phase was characterised by the anticlockwise rotation of the Corsica-Sardinia block, which lasted until the Langhian (ca.16 Ma), and was in turn followed by a slab detachment along the northern African margin. Subsequently, a shift of this active extensional deformation led to the opening of the Tyrrenian basin.
Western Mediterranean[edit]
The Betic-Rif mountain belts developed during Mesozoic and Cenozoic times, as Africa and Iberia converged. Tectonic models for its evolution include: rapid motion of Alboran Domain, subduction zone and radial extensional collapse caused by convective removal of lithospheric mantle. The development of these intramontane Betic and Rif basins led to the onset of two marine gateways which were progressively closed during the late Miocene by an interplay of tectonic and glacio-eustatic processes.
Paleoenvironmental analysis
Its semi-enclosed configuration makes the oceanic gateways critical in controlling circulation and environmental evolution in the Mediterranean Sea. Water circulation patterns are driven by a number of interactive factors, such as climate and bathymetry, which can lead to precipitation of evaporites. During late Miocene times, a so-called "Messinian Salinity Crisis" (MSC hereafter) occurred, where the Mediterranean entirely or almost entirely dried out, which was triggered by the closure of the Atlantic gateway. Evaporites accumulated in the Red Sea Basin (late Miocene), in the Carpatian foredeep (middle Miocene) and in the whole Mediterranean area (Messinian). An accurate age estimate of the MSC—5.96 Ma—has recently been astronomically achieved; furthermore, this event seems to have occurred synchronously. The beginning of the MSC is supposed to have been of tectonic origin; however, an astronomical control (eccentricity) might also have been involved. In the Mediterranean basin, diatomites are regularly found underneath the evaporite deposits, thus suggesting (albeit not clearly so far) a connection between their geneses.
The present-day Atlantic gateway, i.e. the Strait of Gibraltar, finds its origin in the early Pliocene. However, two other connections between the Atlantic Ocean and the Mediterranean Sea existed in the past: the Betic Corridor (southern Spain) and the Rifian Corridor (northern Morocco). The former closed during Tortonian times, thus providing a "Tortonian Salinity Crisis" well before the MSC; the latter closed about 6 Ma, allowing exchanges in the mammal fauna between Africa and Europe. Nowadays, evaporation is more relevant than the water yield supplied by riverine water and precipitation, so that salinity in the Mediterranean is higher than in the Atlantic. These conditions result in the outflow of warm saline Mediterranean deep water across Gibraltar, which is in turn counterbalanced by an inflow of a less saline surface current of cold oceanic water.
The Mediterranean was once thought to be the remnant of the Tethys Ocean. It is now known to be a structurally younger ocean basin known as Neotethys. The Neotethys formed during the Late Triassic and Early Jurassic rifting of the African and Eurasian plates.
Paleoclimate
Because of its latitudinal position and its land-locked configuration, the Mediterranean is especially sensitive to astronomically induced climatic variations, which are well documented in its sedimentary record. Since the Mediterranean is involved in the deposition of eolian dust from the Sahara during dry periods, whereas riverine detrital input prevails during wet ones, the Mediterranean marine sapropel-bearing sequences provide high-resolution climatic information. These data have been employed in reconstructing astronomically calibrated time scales for the last 9 Ma of the Earth's history, helping to constrain the time of past Geomagnetic Reversals.[38] Furthermore, the exceptional accuracy of these paleoclimatic records have improved our knowledge of the Earth's orbital variations in the past.
Ecology and biota
As a result of the drying of the sea during the Messinian salinity crisis,[39] the marine biota of the Mediterranean are derived primarily from the Atlantic Ocean. The North Atlantic is considerably colder and more nutrient-rich than the Mediterranean, and the marine life of the Mediterranean has had to adapt to its differing conditions in the five million years since the basin was reflooded.
The Alboran Sea is a transition zone between the two seas, containing a mix of Mediterranean and Atlantic species. The Alboran Sea has the largest population of Bottlenose Dolphins in the western Mediterranean, is home to the last population of harbour porpoises in the Mediterranean, and is the most important feeding grounds for Loggerhead Sea Turtles in Europe. The Alboran sea also hosts important commercial fisheries, including sardines and swordfish. The Mediterranean monk seals live in the Aegean Sea in Greece. In 2003, the World Wildlife Fund raised concerns about the widespread drift net fishing endangering populations of dolphins, turtles, and other marine animals.
Environmental threats
Biodiversity
Invasive species
The Reticulate whipray is one of the species that colonised the eastern Mediterranean through the Suez Canal.
The opening of the Suez Canal in 1869 created the first salt-water passage between the Mediterranean and Red Sea. The Red Sea is higher than the Eastern Mediterranean, so the canal serves as a tidal strait that pours Red Sea water into the Mediterranean. The Bitter Lakes, which are hyper-saline natural lakes that form part of the canal, blocked the migration of Red Sea species into the Mediterranean for many decades, but as the salinity of the lakes gradually equalized with that of the Red Sea, the barrier to migration was removed, and plants and animals from the Red Sea have begun to colonise the Eastern Mediterranean. The Red Sea is generally saltier and more nutrient-poor than the Atlantic, so the Red Sea species have advantages over Atlantic species in the salty and nutrient-poor Eastern Mediterranean. Accordingly, Red Sea species invade the Mediterranean biota, and not vice versa; this phenomenon is known as the Lessepsian migration (after Ferdinand de Lesseps, the French engineer) or Erythrean invasion. The construction of the Aswan High Dam across the Nile River in the 1960s reduced the inflow of freshwater and nutrient-rich silt from the Nile into the Eastern Mediterranean, making conditions there even more like the Red Sea and worsening the impact of the invasive species.
Invasive species have become a major component of the Mediterranean ecosystem and have serious impacts on the Mediterranean ecology, endangering many local and endemic Mediterranean species. A first look at some groups of exotic species show that more than 70% of the non-indigenous decapods and about 63% of the exotic fishes occurring in the Mediterranean are of Indo Pacific origin,[40] introduced into the Mediterranean through the Suez Canal. This makes the Canal as the first pathway of arrival of "alien" species into the Mediterranean. The impacts of some lessepsian species have proven to be considerable mainly in the Levantine basin of the Mediterranean, where they are replacing native species and becoming a "familiar sight".
According to the International Union for Conservation of Nature definition, as well as Convention on Biological Diversity (CBD) and Ramsar Convention terminologies, they are alien species, as they are non-native (non-indigenous) to the Mediterranean Sea, and they are outside their normal area of distribution which is the Indo-Pacific region. When these species succeed in establishing populations in the Mediterranean sea, compete with and begin to replace native species they are "Alien Invasive Species", as they are an agent of change and a threat to the native biodiversity. In the context of CBD, "introduction" refers to the movement by human agency, indirect or direct, of an alien species outside of its natural range (past or present). The Suez Canal, being an artificial (man made) canal, is a human agency. Lessepsian migrants are therefore "introduced" species (indirect, and unintentional). Whatever wording is chosen, they represent a threat to the native Mediterranean biodiversity, because they are non-indigenous to this sea. In recent years, the Egyptian government's announcement of its intentions to deepen and widen the canal have raised concerns from marine biologists, fearing that such an act will only worsen the invasion of Red Sea species into the Mediterranean, facilitating the crossing of the canal for yet additional species.
Arrival of new tropical Atlantic species
In recent decades, the arrival of exotic species from the tropical Atlantic has become a noticeable feature. Whether this reflects an expansion of the natural area of these species that now enter the Mediterranean through the Gibraltar strait, because of a warming trend of the water caused by Global Warming; or an extension of the maritime traffic; or is simply the result of a more intense scientific investigation, is still an open question. While not as intense as the "lessepsian" movement, the process may be scientific interest and may therefore warrant increased levels of monitoring.
Sea-level rise
By 2100, the overall level of the Mediterranean could rise between 3 to 61 cm (1.2 to 24.0 in) as a result of the effects of climate change.[42] This could have adverse effects on populations across the Mediterranean:
Rising sea levels will submerge parts of Malta. Rising sea levels will also mean rising salt water levels in Malta's groundwater supply and reduce the availability of drinking water.[43]
A 30 cm (12 in) rise in sea level would flood 200 square kilometres (77 sq mi) of the Nile Delta, displacing over 500,000 Egyptians.[44]
Coastal ecosystems also appear to be threatened by sea level rise, especially enclosed seas such as the Baltic, the Mediterranean and the Black Sea. These seas have only small and primarily east-west movement corridors, which may restrict northward displacement of organisms in these areas.[45] Sea level rise for the next century (2100) could be between 30 cm (12 in) and 100 cm (39 in) and temperature shifts of a mere 0.05-0.1°C in the deep sea are sufficient to induce significant changes in species richness and functional diversity.
Pollution
Pollution in this region has been extremely high in recent years.[when?] The United Nations Environment Programme has estimated that 650,000,000 t (720,000,000 short tons) of sewage, 129,000 t (142,000 short tons) of mineral oil, 60,000 t (66,000 short tons) of mercury, 3,800 t (4,200 short tons) of lead and 36,000 t (40,000 short tons) of phosphates are dumped into the Mediterranean each year.[47] The Barcelona Convention aims to 'reduce pollution in the Mediterranean Sea and protect and improve the marine environment in the area, thereby contributing to its sustainable development.'[48] Many marine species have been almost wiped out because of the sea's pollution. One of them is the Mediterranean Monk Seal which is considered to be among the world's most endangered marine mammals.[49]
The Mediterranean is also plagued by marine debris. A 1994 study of the seabed using trawl nets around the coasts of Spain, France and Italy reported a particularly high mean concentration of debris; an average of 1,935 items per km². Plastic debris accounted for 76%, of which 94% was plastic bags.
Shipping
Some of the world's busiest shipping routes are in the Mediterranean Sea. It is estimated that approximately 220,000 merchant vessels of more than 100 tonnes cross the Mediterranean Sea each year—about one third of the world's total merchant shipping. These ships often carry hazardous cargo, which if lost would result in severe damage to the marine environment.
The discharge of chemical tank washings and oily wastes also represent a significant source of marine pollution. The Mediterranean Sea constitutes 0.7% of the global water surface and yet receives seventeen percent of global marine oil pollution. It is estimated that every year between 100,000 t (98,000 long tons) and 150,000 t (150,000 long tons) of crude oil are deliberately released into the sea from shipping activities.
Approximately 370,000,000 t (360,000,000 long tons) of oil are transported annually in the Mediterranean Sea (more than 20% of the world total), with around 250-300 oil tankers crossing the Sea every day. Accidental oil spills happen frequently with an average of 10 spills per year. A major oil spill could occur at any time in any part of the Mediterranean.
Tourism
With a unique combination of pleasant climate, beautiful coastline, rich history and diverse culture the Mediterranean region is the most popular tourist destination in the world—attracting approximately one third of the world's international tourists.
Tourism is one of the most important sources of income for many Mediterranean countries. It also supports small communities in coastal areas and islands by providing alternative sources of income far from urban centres. However, tourism has also played major role in the degradation of the coastal and marine environment. Rapid development has been encouraged by Mediterranean governments to support the large numbers of tourists visiting the region each year. But this has caused serious disturbance to marine habitats such as erosion and pollution in many places along the Mediterranean coasts.
Tourism often concentrates in areas of high natural wealth, causing a serious threat to the habitats of endangered Mediterranean species such as sea turtles and monk seals. Reductions in natural wealth may reduce incentives for tourists to visit
Overfishing
Fish stock levels in the Mediterranean Sea are alarmingly low. The European Environment Agency says that over 65% of all fish stocks in the region are outside safe biological limits and the United Nations Food and Agriculture Organisation, that some of the most important fisheries—such as albacore and bluefin tuna, hake, marlin, swordfish, red mullet and sea bream—are threatened.[date missing]
There are clear indications that catch size and quality have declined, often dramatically, and in many areas larger and longer-lived species have disappeared entirely from commercial catches.
Large open water fish like tuna have been a shared fisheries resource for thousands of years but the stocks are now dangerously low. In 1999, Greenpeace published a report revealing that the amount of bluefin tuna in the Mediterranean had decreased by over 80% in the previous 20 years and government scientists warn that without immediate action the stock will collapse.
Aquacultur
Aquaculture is expanding rapidly—often without proper environmental assessment—and currently accounts for 30% of the fish protein consumed worldwide. The industry claims that farmed seafood lessens the pressure on wild fish stocks, yet many of the farmed species are carnivorous, consuming up to five times their weight in wild fish.
Mediterranean coastal areas are already over exposed to human influence, with pristine areas becoming ever scarcer. The aquaculture sector adds to this pressure, requiring areas of high water quality to set up farms. The installation of fish farms close to vulnerable and important habitats such as seagrass meadows is particularly concerning.
A typical October morning starts above the local fields of Siilinjärvi, where autumn's appearance has set a silence on the rural environment. That silence is broken down as the freight train from Pyhäsalmi arrives at Siilinjärvi and soon its separated approach puts the train with class Dv12s on the final stretch of the journey.
The Moravian–Silesian Beskids (Czech: Moravskoslezské Beskydy, Slovak: Moravsko-sliezske Beskydy) is a mountain range in the Czech Republic with a small part reaching to Slovakia. It lies on the historical division between Moravia and Silesia, hence the name. It is part of the Western Beskids, which is in turn part of the Outer Western Carpathians.
The mountains were created during the Alpine Orogeny in the Tertiary. Geologically, they consist mainly of flysch deposits. In the north, they steeply rise nearly 1,000 m (3,300 ft) over a rather flat landscape; in the south, they slowly merge with the Javorníky. In the south-west, they are separated from the Vsetínské vrchy by the Rožnovská Bečva valley; in the north-east, the Jablunkov Pass separates them from the Silesian Beskids.
The highest point is Lysá hora mountain at 1,323 m (4,341 ft), which is one of the rainiest places in the Czech Republic with around 1,500 mm (60 in) of precipitation a year. Many legends are bound to Radhošť Mountain, 1,129 m (3,704 ft), which is one of the most visited places in the mountains together with the nearby Pustevny resort.
The Moravian-Silesian Beskids create the largest part of the Beskydy Landscape Protected Area (Czech: Chráněná krajinná oblast Beskydy or Czech: CHKO Beskydy for short). The mountains are 80% forested, though mainly by plantations of spruce which were in some parts severely damaged by emissions from the Ostrava industrial region. Originally, the mountains were covered by mixed forest with dominant beech which are preserved in many places. Recently, permanent occurrence of all three large Central European carnivours – lynx, bear and wolf – have been confirmed in the area.
(Wikipedia)
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During last October, we did another autumn pro-longed weekend hike across the eastern part of the Moravian–Silesian Beskids, which is far much less visited that its western part - nice weather, fine views, solitude, and lots of freedom - it's an area definitely worth visiting and exploration.
This time, the itinerary was as follows: Mosty u Jablunkova -> Skalka -> Úplaz -> Mionší -> Kamenitý -> Kozubová -> Návsí -> Filipka -> Velký Stožek -> Velký Sošek -> Velká Čantoryje -> Nýdek.
Taken below the Kamenitý hill and hut.
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Slender trees with white bark, possibly a species of birch, used to separate two pastures at my former home in Charlotte Court House, Virginia.
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Jewish patients’ graves, clustered off to the side in the cemetery of the old Matteawan State Hospital for the Criminally Insane in what is now the city of Beacon, N.Y.
In the beginning, God created the heavens and the earth. The earth was without form and void, and darkness was over the face of the deep. And the Spirit of God was hovering over the face of the waters. And God said, “Let there be light,” and there was light. And God saw that the light was good. And God separated the light from the darkness. God called the light Day, and the darkness he called Night. And there was evening and there was morning, the first day.
Driving on Snake Road I saw a gang of Wild Turkeys (about 20). Stopped the car, by the time I got back to the spot the turkeys where small dots in the viewfinder. But this one was on the wrong side of the fence.
LAKHTA
.This small village on the northern shore of the Gulf of Finland, about 15 km northwest of the city, is home to human settlements on the banks of the Neva. It was on the territory of Lakhta that the remains of a man’s parking site of three thousand years ago were found.
In official documents, a settlement named Lakhta dates back to 1500. The name is derived from the Finnish-speaking word lahti - "bay". This is one of the few settlements that has not changed its name throughout its 500-year history. Also known as Laches, Lahes-by, Lahes and was originally inhabited by Izhora. In the last decades of the 15th century, Lakhta was a village (which indicates a significant population) and was the center of the eponymous grand-parish volost, which was part of the Spassko-Gorodensky graveyard of the Orekhovsky district of the Vodskaya Pyatina. In the village, there were 10 courtyards with 20 people (married men). In Lakhta, on average, there were 2 families per yard, and the total population of the village probably reached 75 people.
From the notes on the margins of the Swedish scribe book of the Spassky graveyard of 1640, it follows that the lands along the lower reaches of the Neva River and parts of the Gulf of Finland, including Lakhta Karelskaya, Perekulya (from the Finnish “back village”, probably because of its position relative to Lakhti) and Konduy Lakhtinsky, were royal by letter of honor on January 15, 1638 transferred to the possession of the Stockholm dignitary, Rickschulz general Bernhard Sten von Stenhausen, a Dutchman by birth. On October 31, 1648, the Swedish government granted these lands to the city of Nyuen (Nyenschanz). With the arrival of the Swedes in Prievye, Lakhta was settled by the Finns, who until the middle of the 20th century made up the vast majority of the villagers.
On December 22, 1766, Catherine 2 granted Lakhta Manor, which was then in the Office of the Chancellery from the buildings of palaces and gardens, "in which and in her villages with courtyards 208 souls," her favorite Count Orlov. Not later than 1768, Count J.A. Bruce took over the estate. In 1788, Lakhta Manor was listed behind him with wooden services on a dry land (high place) and the villages Lakhta, Dubki, Lisiy Nos and Konnaya belonging to it also on dry land, in those villages of male peasants 238 souls. On May 1, 1813, Lakhta passed into the possession of the landowners of the Yakovlevs. On October 5, 1844, Count A.I. Stenbok-Fermor entered into the possession of the Lakhtinsky estate, which then had 255 male souls. This clan was the owner of the estate until 1912, when its last representative got into debt and noble custody was established over the estate. On October 4, 1913, in order to pay off his debts, he was forced to go for corporatization, and the Lakhta estate passed into the ownership of the Joint Stock Company “Lakhta” of Count Stenbock-Fermor and Co.
After the revolution, Lakhta was left on its own for a while, here on the former estate of the counts Stenbock-Fermorov on May 19, 1919, the Lakhta excursion station was opened, which existed there until 1932. In the early 1920s, sand mining began on Lakhta beaches, and the abandoned and dilapidated peat plant of the Lakhta estate in 1922 took over the Oblzemotdel and put it into operation after major repairs. In 1963, the village of Lakhta was included in the Zhdanovsky (Primorsky) district of Leningrad (St. Petersburg).
At the beginning of Lakhtinsky Prospekt, on the banks of the Lakhtinsky spill, there was the village of Rakhilax (Rahilax-hof, Rahila, Rokhnovo). Most likely, under this name only one or several courtyards are designated. There is an assumption that the name of the village was formed from the Finnish raahata - “drag, drag,” because there could be a place for transportation through the isthmus of the Lakhtinsky spill (we should not forget that not only the bridge over the channel connecting the spill with the Gulf of Finland was not yet here, the duct itself was many times wider than the current one). The search book of the Spassko-Gorodensky graveyard of 1573, describing the Lakhta lands, mentions that there were 2 lodges in the “Rovgunov” village, from which we can conclude that we are talking about the village of Rohilaks, which the Russian scribes remade into a more understandable to them Rovgunovo. The village was empty in Swedish time and was counted as a wasteland of the village of Lahta.
On the banks of the Lakhtinsky spill, near the confluence of the Yuntolovka River, from the 17th century there existed the village of Bobylka (Bobylskaya), which merged into the village of Olgino only at the beginning of the 20th century, but was found on maps until the 1930s. It is probably the Search Book that mentions it Spassko-Gorodensky churchyard in 1573 as a village "in Lakhta in Perekui", behind which there was 1 obzh. With the arrival of the Swedes by royal letter on January 15, 1638, the village was transferred to the possession of the Stockholm dignitary, Rickshaw General Bernhard Sten von Stenhausen, a Dutchman by birth. On October 31, 1648, the Swedish government granted Lahti lands to the city of Nyuen (Nyenschanz). On the Swedish map of the 1670s, in the place of the village of Bobylsky, the village of Lahakeülä is marked (küla - the village (Fin.)). The village could subsequently be called Bobyl from the Russian word "bobyl."
The owners of Bobylskaya were both Count Orlov, and Count Y. A. Bruce, and the landowners Yakovlev. In 1844, Count A.I. Stenbok-Fermor entered into the possession of the Lakhtinsky estate (which included the village of Bobyl). This family was the owner of the estate until 1913, when the owners, in order to pay off their debts, had to go for corporatization, and the Lakhta estate was transferred to the ownership of the Lakhta Joint-Stock Company of Count Stenbock-Fermor and Co. By the middle of the 20th century, the village merged with the village of Lakhta.
The name Konnaya Lakhta (Konnaya) has been known since the 16th century, although earlier it sounded like Konduya (Konduya Lakhtinskaya) or just Kondu (from the Finnish kontu - courtyard, manor). Subsequently, this name was replaced by the more familiar Russian ear with the word "Horse". In the Search Book of the Spassko-Gorodensky Pogost in 1573, it is mentioned as the village "on Kovdui", where 1 obzh was listed, which indicates that there most likely was one yard. On January 15, 1638, together with neighboring villages, it was transferred to the possession of the Stockholm dignitary, Rickschulz General Bernhard Steen von Stenhausen, of Dutch origin. On October 31, 1648, the Swedish government granted these lands to the city of Nyuen (Nyenschanz). In a deed of gift, Konduya Lakhtinskaya is called a village, which indicates a noticeable increase in its population. Later, on the Swedish map of the 1670s, on the site of the present Horse Lahti, the village of Konda-bai is marked (by - village (sv)).
The owners of Konnaya Lakhta, as well as the villages of Bobylskaya and Lakhta, were in turn Count Orlov, Count Ya. A. Bruce, and the landowners Yakovlev. In 1844, Count A.I. Stenbok-Fermor entered the possession of the Lakhta estate (which included Konnaya Lakhta. This family was the owner of the estate until 1913, when the owners had to go to corporations to pay off their debts, and the Lakhta estate became the property of Lakhta Joint Stock Company of Count Stenbock-Fermor and Co. In 1963, Horse Lahta was included in the Zhdanov (Primorsky) district of Leningrad (St. Petersburg).
As the dacha village of Olgino appeared at the end of the 19th century and initially consisted of both Olgin itself and the villages of Vladimirovka (now part of Lisiy Nos) and Aleksandrovka. In the first half of the 18th century, this territory was part of the Verpelev palace estate, which in the second half of the 18th century was granted to Count G. G. Orlov, then it was owned by the family of landowners the Yakovlevs, in the middle of the 19th century the estate was transferred to the counts of Stenbock-Fermor. In 1905 A.V. Stenbok-Fermor, the then owner of Lakhta lands, divided the lands around Lakhta into separate plots with the intention of selling them profitably for dachas. So there were the villages of Olgino (named after the wife of Olga Platonovna), Vladimirovka (in honor of the father of the owner; the coastal part of the modern village of Lisy Nos) and Alexandrov or Aleksandrovskaya (in honor of Alexander Vladimirovich himself). It is likely that on the site of the village was the village of Olushino (Olushino odhe) - a search book of the Spassko-Gorodensky churchyard in 1573 mentions that there were 1 obzh in the village of Olushkov’s, which suggests that at least one residential the yard. On behalf of Olushka (Olpherius). Most likely, the village was deserted in Swedish time and then was already listed as a wasteland belonging to the village of Lahta. Thus, the name of the village could be given in harmony with the name of the mistress and the old name of the village.
The villages were planned among a sparse pine forest (the layout was preserved almost unchanged), so there were more amenities for living and spending time there than in Lakhta. A park was set up here, a summer theater, a sports ("gymnastic") playground, a tennis court, and a yacht club were arranged.
In the 1910s about 150 winter cottages were built in Olgino, many of which are striking monuments of "summer cottage" architecture. In 1963, the village of Olgino was included in the Zhdanovsky (Primorsky) district of Leningrad (St. Petersburg).
Near Olgino, in the area of the Dubki park, there was a small village Verpeleva (Verpelevo), which consisted of only a few yards. In the first half of the XVIII century. this territory was part of the palace estate "Verpeleva", which in the second half of the XVIII century. It was granted to Count G. G. Orlov, then passed to the Counts of Stenbock-Fermor. The village has not existed for a long time, but the entire reed-covered peninsula (barely protruding above the water of the Verpier-Luda peninsula (Verper Luda (from the Finnish luoto - “small rocky island”)) still existed, and there was another spelling the name of this island is Var Pala Ludo).
Kamenka. The Novgorod scribal book mentions two villages in the Lakhta region with a similar name, referring to the possessions of Selivan Zakharov, son of Okhten, with his son and 5 other co-owners. On the lands of this small patrimony, which, unlike the estate was inherited, peasants lived in 3 villages, including: the village "Kamenka in Lakhta near the sea" in 5 yards with 5 people and arable land in 1,5 obzhi, the village "on Kamenka "in 2 courtyards with 2 people and arable land in 1 obzhu. For the use of land, the peasants paid the owners of the patrimony 16 money and gave 1/3 of the rye harvest. Thus, in the 16th century on the Kamenka River (another name for the Kiviyoki River, which is the literal translation of kivi - "stone", joki - "river") there was one large village of Kamenka near its confluence with the Lakhtinsky spill and the second, smaller, somewhere upstream. On the drawing of Izhora land in 1705, a village under this name is depicted in the area of the modern village of Kamenka. The village of Kamennaya in the middle reaches of Kamenka and on the map of 1792 is designated. Other name options are Kaumenkka, Kiviaja.
In the second half of the 18th century, Kamenka became a vacation spot for Russian Germans. Here in 1865, German colonists founded their "daughter" colony on leased land. Since then, the village has received the name Kamenka Colony (so called until the 1930s). In 1892, a colony near the village of Volkovo "budded" from it. The inhabitants of both colonies belonged to the Novo-Saratov parish and since 1871 had a prayer house in Kamenka, which was visited by 250 people. He maintained a school for 40 students. The house was closed in 1935 and later demolished.
Currently, Kamenka exists as a holiday village, located along the road to Levashovo. Since 1961 - in the city, part of the planning area in the North-West, from the mid-1990s. built up with multi-storey residential buildings and cottages.
Volkovo. The settlement is about southeast of the village of Kamenka - on the old road to Kamenka, on the bank of a stream that flows into Kamenka between the village of Kamenka and the Shuvalovsky quarry. In 1892, a German colony emerged on the territory of the village, "budding" from a nearby colony in the village of Kamenka. The origin of Volkovo is not clear, the village is found only on maps of 1912, 1930, 1939, 1943. and probably appeared no earlier than the 19th century.
Kolomyagi. Scribe books of the XV — XVI centuries and Swedish plans testify that small settlements already existed on the site of Kolomyag. Most likely, these were first Izhora or Karelian, then Finnish farms, which were empty during the hostilities of the late XVII century.
The name "Kolomyag" connoisseurs decipher in different ways. Some say that it came from the "colo" - in Finnish cave and "pulp" - a hill, a hill. The village is located on the hills, and such an interpretation is quite acceptable. Others look for the root of the name in the Finnish word "koaa" - bark - and believe that trees were processed here after felling. Another version of the origin of the name from the Finnish "kello" is the bell, and it is associated not with the feature of the mountain, but with the "bell on the mountain" - a tower with a signal bell standing on a hill.
The owners of Kolomyazhsky lands were Admiral General A.I. Osterman, Count A.P. Bestuzhev-Ryumin, a family of Volkonsky. In 1789, the Volkonskys sold these lands to retired colonel Sergei Savvich Yakovlev. On his estate S. S. Yakovlev built a manor and lived in it with his wife and seven daughters. The once-Finnish population of Kolomyag was “Russified” by that time - it was made up of descendants of serfs resettled by Osterman and Bestuzhev-Rumin from their villages in Central Russia (natives of the Volga and Galich) and Ukraine. Then the name "Kellomyaki" began to sound in Russian fashion - "Kolomyagi", although later the old name also existed, especially among local Finns. And not without reason the indigenous Kolomozhites associate their origin with the Volga places, and the southern half of the village is now called “Galician”.
Yakovlev died in 1818. Five years after his death, a division of the territory of the manor was made. The village of Kolomyagi was divided in half between two of his daughters. The border was the Bezymyanny stream. The southeastern part of the village of Kolomyagi beyond Bezymyanny creek and a plot on the banks of the Bolshaya Nevka passed to the daughter Ekaterina Sergeevna Avdulina.
Daughter Yakovleva Elena Sergeevna - the wife of General Alexei Petrovich Nikitin, a hero of the Patriotic War of 1812, who was awarded the highest military orders and twice a gold sword with the inscription "For courage", died early, leaving her daughter Elizabeth. The northwestern part of Kolomyag inherited the young Elizabeth, so this part of Kolomyag was practically inherited by the father of Yakovlev’s granddaughter, Count A.P. Nikitin, who in 1832 became the owner of the entire village. It is his name that is stored in the names of the streets - 1st and 2nd Nikitinsky and Novo-Nikitinsky. The new owner built a stone mansion on the estate’s estate - an excellent example of classicism of the first third of the 19th century, which became his country house and has survived to this day and has been occupied until recently by the Nursing Home. It is believed that this mansion was built according to the project of the famous architect A.I. Melnikov. The severity and modesty of the architectural appearance of the facades and residential chambers of the Nikitin mansion was opposed by the splendor of ceremonial interiors, in particular the two-light dance hall with choirs for musicians. Unfortunately, with repeated alterations and repairs, many details of the decor and stucco emblems of the owners disappeared. Only two photographs of the 1920s and preserved fragments of ornamental molding and paintings on the walls and ceiling show the past richness of the decorative decoration of this architectural monument. The mansion was surrounded by a small park. In it stood a stone pagan woman brought from the southern steppes of Russia (transferred to the Hermitage), and a pond with a plakun waterfall was built. Near the pond there was a "walk of love" from the "paradise" apple trees - it was called so because the bride and groom passed through it after the wedding. Here, in the shadow of these apple trees, young lovers made appointments.
Under the Orlov-Denisov opposite the mansion (now Main Street, 29), the structures of an agricultural farm were erected, partially preserved to this day, and the greenhouse. Behind the farm were the master's fields. On them, as the New Time newspaper reported in August 1880, they tested the reaping and shearing machines brought from America.
In the 19th century, the provincial surveyor Zaitsev submitted for approval the highway called the Kolomyagskoye Shosse. The route was supposed to connect the village, gradually gaining fame as a summer residence of the "middle arm", with St. Petersburg. The construction of the road ended in the 1840s, and then horse-drawn and country-house crafts became the most important articles of peasant income. In addition, peasants either built small dachas in their yards, or rented their huts for the summer. Located away from the roads, surrounded by fields, the village was chosen by multi-family citizens.
The income from the summer cottage industry increased from year to year, which was facilitated by the summer movement of omnibuses that opened on the new highway from the City Council building. They walked four times a day, each accommodated 16 people, the fare cost 15 kopecks. Even when the Finnish Railway with the nearest Udelnaya station came into operation in 1870, the highway remained the main access road through which public carriages pulled by a trio of horses ran from the Stroganov (now Ushakovsky) bridge.
So here we go again! Another fun entry of 'Andrew reads old-as-dirt comic books', an ongoing series! :P
The story starts off with this scrub of a college-football-playing science nerd trying to take Joan (no last name because she was a fictional woman in the 40's) on a date. She then turns him down by saying that he sucks and she's already taken.
So Jay is all like, “Yeah good point, I'm gonna work extra hard today instead” so he goes to the field and still sucks, then he later goes to his science class and falls asleep on the job waking up at three thirty in the morning because he was waiting on separating the elements of hard water... yeah idk man.
Anyway, like a doofus, he lights up a cigarette in the lab to take a break, leans his back onto his desk, and ends up knocking all of those elements onto the floor, leading the fumes to cause him to pass out.
So he's found later by his professor, who rushes him to a hospital where he stay's unconscious for a few weeks. Then there's a few panels of unsupported scientific exposition of two scientists talking out their asses about how Hard Water is a real thing and it gives people super speed if Jay EVEN SURVIVES (dun dun dun)
But meanwhile in the other room Jay is up and about and he just happens to see Joan No-Last-Name walking outside the window and Jay's all like “Holy hard water it's that chick who said no to me!” and then without realizing it, he zips outside in... you guessed it... a flash (whomp whomp)
Outside Joan is all like “Woah where did you come from, also I'm going to the library” to which Jay is all like “nbd dude, I got you” and he zips over to the library and harasses a lady to stamp the book Joan wants.
Jay's then back in a jiff and Joan is all like “what the heck man” to which Jay responds with, and I kid you not “It scares me. I'm just a freak of science. Anyhow, will you go on that dance with me now?”
Despite all the red-flags, Joan says yes because this was the 40s... oof.
Later at the football field Jay is all like “put me in coach” and the coach is all like “fine I guess, btw you suck Jay” and then like Andrew Garfield in The Amazing Spider-Man 1, uses his powers like an idiot in front of hundreds of people in the stadium.
Apparently there's no repercussions over it and no one else remembers this at all because the next few panels are of Jay graduating college and reading the newspaper about some crooks doing some crime stuff.
Later Joan shows up at Jay's place and watches him play tennis with himself and is all like “hey man, my Dad's been kidnapped, could you like help maybe?” Then as they're chatting, a drive-by shooter fires off a shot at Joan, to which Jay saves the day by catching the bullet mid-air!
Cut to the shooter walking into his hideout being like “Yeah guys she'd dead I shot her, no way anybody else could have caught a bullet and saved her, anyway how's her Dad doing in the mirror torture room we tossed him in?”
Cut to Dad-Joan who's like “gah my eyes too many mirrors! Btw I'm still not telling you my secrets to my Atomic Bombarder! Gah! Mirrors! Gasp!”
The crook is all like “hmm maybe if I go get Joan's body we can get some info” so like an idiot he returns to the crime scene, bumps into Jay, asks were the dead girl is, and Jay is all like “Huh... he knows something about something...” Then Joan comes out is all “Hello shady stranger, I'm Joan and I'm very alive!” Then the dude is all like “Uh yeah peace out” and bails.
So Jay trails him back to the bad guy lair penthouse place and is like “He crooks, stop your crime! Also it's me The Flash and I have a cool costume now!” and then he catches some more bullets, finds Mr Atomic JoanDad and hightails it out of there to drop him off at home before going back to the bad guy mansion again later.
(are you all ready for this to be over because I sure am)
Anyway he hides behind a curtain and overhears their entire plan to take a fighter plane out and shoot everybody on Coney Island while also kidnapping Joan and DadJoan again (this time v quietly)
Naturally Jay is like, not on your life! (but instead of stopping it right then and there) he waits till the attack the next day and shows off a spectacle of powers, catching all the bullets from the plane's machine gun, then zipping across town to stop the kidnapping. Then after killing his partners, one of the bad guy's gets away in a new extra fast getaway car that's SO fast that he can't control how fast it is when taking a tight cliff-side turn because Jay spooked him because he was just that fast.
Get it guys? He's the flash! He goes quick! He's speedy! So swift! Wow!
Anyway, the goon goes over the edge in his car, and Jay doesn't even attempt to save him, but instead beats the car to the bottom of the ravine to gloat about how he stopped the goons as the car comes to a smoldering halt. Classic hero work.
Then the last three panels (because there wasn't enough story already) Mr Joan is all like “man that Flash guy... wonder who he is under that helmet... he wasn't even wearing a mask or anything! I'm just stumped Jay! Who could he be?!”
To which Joan is all “idk Dad, oh by the way Garrick, you killed a man and your secret is safe with me! *wink*!”
Geez, Gardner Fox was a wordy guy...
***
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Kasper knit pink/black and white jacket, pink pencil skirt. Hanes hose, JCP Charles white patent bow vamp pumps. Faceapp used for makeup and hair.
Previous set from Duga here: www.flickr.com/photos/timster1973/sets/72157643924793935/
Duga-3 (NATO reporting name Steel Yard) was a Soviet over-the-horizon radar system. It was developed for the Soviet ABM early-warning network. The system operated from 1976 to 1989. Its distinctive and mysterious shortwave radio signal came to be known in the west as the Russian Woodpecker.
Two stations of Duga-3 were installed: a western system around Chernobyl and an eastern system in Siberia.
The transmitter for the western Duga-3 was located a few kilometers southwest of Chernobyl (south of Minsk, northwest of Kiev). The receiver was located about 50 km northeast of Chernobyl (just west of Chernihiv, south of Gomel).
The Soviets had been working on early warning radar for their anti-ballistic missile systems through the 1960s, but most of these had been line-of-sight systems that were useful for raid analysis and interception only. None of these systems had the capability to provide early warning of a launch, which would give the defenses time to study the attack and plan a response. At the time the Soviet early-warning satellite network was not well developed, and there were questions about their ability to operate in a hostile environment including anti-satellite efforts. An over-the-horizon radar sited in the USSR would not have any of these problems, and work on such a system for this associated role started in the late 1960s. Duga-3 could detect submarines and missile launches in all of Europe and the Eastern coast of United States.
The first experimental system, Duga-1, was built outside Mykolaiv in Ukraine, successfully detecting rocket launches from Baikonur Cosmodrome at 2,500 kilometers. This was followed by the prototype Duga-2, built on the same site, which was able to track launches from the far east and submarines in the Pacific Ocean as the missiles flew towards Novaya Zemlya. Both of these radar systems were aimed east and were fairly low power, but with the concept proven work began on an operational system. The new Duga-3 systems used a transmitter and receiver separated by about 60 km.
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Only a couple of inches of glass separated young man from cold deep space abyss. He almost stuck to the illuminator and was looking at blue globe of home planet. He was lucky to born here on one of terraformed planets, but not on some piece of rock with poisoned atmosphere. Carthage was “green” earth type planet, however it wasn’t good developed as similar ones. There were only a few cities and some green fields. Farming was the main business there.
And now he was leaving home planet. There were no trees, no grass, no wind, and even no ground around. And that was uncomfortable. Wires buzzed somewhere. Some machines made quite noise. Some vibration appeared –main engine was switched on. And suddenly starship’s frame started to howl, like it was alive. A very strange feeling.
–Hey, don’t be afraid, man. The ship wouldn’t blow up, – a man with short black beard opened the door. – Just beams are creaking. That’s usual.
–Wait, what are you doing here in my cabin and who are you?
–Frank. Looks like I’m your fellow traveler.
–Uhm, I’ve got agreement with captain. I must be alone here.
–So there are more special passengers than expected. As you see there are too many people on this ship. You are lucky to get this personal cabin but not public one. That’s not good to live near that scum. But I’m a good man, – Frank tried to make nice face.
–Scum? You are calling these people scum just because they live in colonies?
–Trust me, I know that. I was born in Outer world colony. But they are mostly from New-London. It was good colony when mines worked. Now it’s heaven for drug dealers, killers, robbers and bandits. It’s easier to find a virgin in brothel than an honest man there. Anyway, what’s your name?
–Jacques, – they shook hands.
–So, is it your first flight? You look nervous.
–I often fly to moon, but I’ve never been in another star system. Only in childhood. I think you have more experience.
–Yes, I’ve been always working in space as repair engineer. I visited almost every inhabited system. Maybe. You should not worry. I took part in replacing reactor here. This is good ship, not new but reliable.
–What has happened with old reactor? As I know, they can work for a long time.
–Looks like you have some knowledge about this stuff.
–Not much. “The Ark”, ship that delivered first colonists to Carthage was broken long time ago, but it’s reactor still working on the planet.
–Yes, that’s possible, but only the core can work so long. I’m sure other reactor systems were replaced many times. So about this ship. It’s owner lost his license and he had so set up weaker reactor.
–Oh, that law about long-range transporting is real headache. My family grows grain for colonies. Not much. So big ships are useless for as for transporting, we have to hire small ones. But this law causes so many problems… It’s very hard to find someone with license.
–This ship was transporting ore from Outer world. Now it’s some kind of space bus. Damn bureaucrats. Long hyperjumps are risky a bit. And reliable crew is important. But in fact this law protects large transportation corporations. In Outer worlds nobody cares about license, but there is no job for ore transporter if you are not going to haul it to the Inner ones, where license is needed.
–I know that Outer worlds buy food and sell ore. Something like that. There are mostly mining colonies and they almost don’t trade with each other.
–Oh you know nothing. There are not only mines, but many industrial worlds. They just don’t like strangers. And why they should? Federation banned all trade except ore and food. Have you heared about that? Anyway, why is it grain? It’s more profitable and easier to product biomass.
–There is good demand for normal natural food. Yes it’s harder to find customer and it’s harder to grow it. But there are some people in colonies who want to pay for real bread but not those synthetic nutritious bricks. So why not? And are you working on this ship?
–Indeed, natural food is so expensive. Almost all of it is made for rich, and colonies get nothing. So that’s a good deal to grow grain for colonies. However, it’s impossible to feed everyone only with natural food. It’s easier to make synthetic one. And it’s health anyway. Not expensive. But sometimes I really want to eat some real apple. “Green” world become so rich because colonies depend on their food supplies. And when they have some argues, greens just raise the price. Bastards… Oh no, I not working here. I had a rest on Carthage and now I’m going back to Helen colony. There are huge shipyards where I’m working now. To be honest, I’m tired of working on ships during flight. Do you imagine how dangerous is it to repair ship in deep space? If something breaks it breaks suddenly. And it causes additional damage as rule. For example power distributor burns down. Because of it reactor coolers break. Or hyperdrive becomes overloaded. Something like that. And you must repair as soon as possible. Your life depends on it. There was accident on liner. Food processor fired. Thing which makes those very tasty snot, which people call nutritious gel. So canteen burns. And ship AI doesn’t allow to depressurize bay to stop fire. And do you know why? It mixed up that snot with people. Organic sensors were calibrated poorly. And now think what will happen if reactor blow up?
–I think you will be dead anyway. So, are problems with AI take place often?
–In fact, you can survive even after explosion of reactor. There are so many protection systems that shoot it down in a moment in case of failure. So it almost can’t explode strongly. Yes there will be hard damage. The ship will stay in one piece. The only way to make real fireworks is to overload it and switch off all protection systems. No, there are almost no problems with AI. Usually it’s isolated from main system and it is used for navigation and so on. Hm, you should know something about mad AI, don’t you? That accident on “Carthage”.
–Yes that Ark called Carthage did hyperjump and something exploded heavily. All main crew died. And AI didn’t wake reserve crew. It started act by itself and continued travelling in order to find ideal planet for colonists. Also life support system was damaged. There was almost suitable planet nearby. But it wanted to find ideal one. So AI killed one half of people to save the others. 50 millions of lives. At the end it found this planet. But who knows what exactly happened here? It was so long time ago. Did you choose shipyards just because it’s safety there?
–I also had some problems with the law. I took part in both civil wars in some way on both sides. So sometimes someone remembers it. All in all it’s better to live in colony, than always travel in space. I’ve already seen this world. So I want to have some rest. Life on starship isn’t nice. Radiation. Awful food. Smell. Do you know how does they restore oxygen? Hydraponics can be set up only on a big ship. Biorector does it. Smart bacteria eat biowaste, carbon dioxide and heat, than produce oxygen and protein food. Oh that smell. You can feel it if air filters broke. And you can feel it even if they work properly. But if bioreactor breaks…
–So you were soldier. I didn’t think I can meet someone like you. That’s rare profession nowadays.
–No, no. I was a civil technician on military starship. And only twice I saw a battle. You know, now I hate battleships. Civil ones are so convenient, so much space. Half of bays on military ones doesn’t have air. You always must wear spacesuit. Corridors are so narrow. Almost no artificial gravity. Yes it is needed to survive in battle, but no one can make me fly on this thing anymore.
–Does it happen every time? I mean accidents. To be honest, I can’t understand how you can repair engine, for example. It’s so complicated for me.
–No. Time to time. Usually that’s some small failures, which are easy to fix. To be honest, that’s no so dangerous. There are so many protection systems, reserve systems and so on. Disasters are very rare nowadays. How do I repair reactor? With help of mounting and someone’s mother. He-he. Yes starship is very complicated. But it is designed to be repaired easily. Simple things break first. Wires can burn down. Or a tube leaks. I hope you understand the idea. By the way engine isn’t so complicated. But bioreactor does. I should say sometimes you must be afraid of people not the machines. There are mercenaries in cargo bay. Who knows what they can do. Stay out of them. Looks like you are tired of conversations. I’ll go and eat something.
'Actually,' she said, 'I'm separated.'
A class of dizziness palpable from the high stool the other side of me.
'I'm sorry to hear that,' whispered Mr Kelliher, decorous again after his cheeky intrusion.
'Ah,' she said. 'It's the way things work out sometimes.'
We nodded, the three men, sombre as owls. We nodded as though the cruel variables of love were hardly news to us. We nodded as though we'd each known heartbreak and the ache of a lost love, as though we'd each walked the Castle Walk, at four in the morning, in cold rain, with the collars turned up against a lonely wind. Oh what we wouldn't have given for broken hearts.
Excerpt from Breakfast Wine, from There are little kingdoms, a great collection of short stories by Kevin Barry.
Explore #94, 17th Oct '08! My highest Explore yet. View large.
New separate hip and butt pads figure enhancement regime. Brava and muchas gracias to Pam Sashaa for the concept which she demonstrates in this excellent video... www.youtube.com/watch?v=CfRo44BQkW4
All pads are made out of 5cm thick foam. Hip pads are 60cm tall and 38cm wide and made out of medium to firm density foam, and the butt pads are 28cm round and also made out of medium to firm density foam. The calf pads are made out of spare (old butt pads!) soft to medium density foam and are scooped out a little to accommodate my own calf muscle. This padding regime will give you a much nicer and more realistic derrière than using one piece hip and butt pads, as you are about to see... So lets get started!!!
See the next two photos for the application of these pads.
January 2022 - I have since made longer and wider hip and butt pads and will do another tutorial at some stage...
I really felt like this when I snapped the photo. I think the sympathy was mutual for me and this feather
Agfa Viking. Fuji Provia 100 (pushed to 400).
5 Separate shoots
5 Locations
5 Wardrobe/Make up/Hair changes
5 Types of film (Polaroid Type 667, Polaroid Type 779, Agfa Portrait 160, Fuji Provia 100, Kodak Tri-X 320)
5 Cameras (Polaroid 600 SE, Polaroid SX-70, Zeiss Ikon Ikoflex II, Agfa Viking, Kodak Brownie Reflex 20)
Only allowed 2 shots with each camera.
Model, make-up & hair, it's all Lauren. You can visit her make-up/hair Model Mayhem page here.
**Last photo of Project 5. Thanks for sharing this with me.**