Mick Harper wrote: Let's do some field trials!
Too late! You'll just get us in trouble with the spider-hugging local authority.
Mick Harper wrote: Let's do some field trials!
Portugal: the country has no rias as such: the Ria de Aveiro in Aveiro, and Ria Formosa in Eastern Algarve are actually lagoons.
The word ria comes from Portuguese ria or Galician ría, which is related to Spanish and Galician río and Portuguese rio (river). Rias are present all along the Galician coast in Spain. As originally defined, the term was restricted to drowned river valleys cut parallel to the structure of the country rock that was at right angles to the coastline. However, the definition of ria was later expanded to other flooded river valleys regardless of the structure of the country rock.
England: The south coast of England is a submergent coastline which contains many rias, including Portsmouth Harbour, Langstone Harbour, Chichester Harbour, Pagham Harbour, Southampton Water, Poole Harbour, the estuaries of the Exe, Teign and Dart, then Kingsbridge Estuary, Plymouth Sound in Devon, and the estuaries of the River Fowey, River Fal and Helford River in Cornwall. On the north coast is the River Camel and the River Taw. In Essex is the Blackwater River and River Crouch. The River Severn also forms a large ria.
Its rich mineral deposits of tin and gold led to the development of Bronze Age metallurgy, and to the commerce of bronze and gold items all along the Atlantic coast of Western Europe. A shared elite culture evolved in this region during the Atlantic Bronze Age.
After classical authors, we have to wait until the 18 th c. and the Enlightenment to find
some works which give us concrete data about tin mining in our area. Cornide Saavedra
y Folgueira is the oldest author whose work was accessible 5 . He did not questioned the
classical texts, and give some examples of tin mining places from Galicia or Northern
Portugal. We realize that very few tin deposits were known in that time: he noticed only
3. It seems that people had forgotten where the tin was mined in NW Iberia. We will
have to wait the end of the 19 th c. to find more information about tin deposits, from an
English mining engineer who worked in our area: Borlase 6 . The number of known sites has
increased since the second half of the 19 th and made him accept than classical authors
were right when they wrote NW Iberia was a wealthy tin producer. In the beginning of the
20 th c., the abbot Alves redacted an encyclopedic work, Memorias arqueológico-historicas
do distrito de Bragança 7 , whose second volume deals with mineral resources from his area.
This book really provides a lot of data, although the chronology indicated is sometimes
quite vague.
Continuing in the 20 th c., most of the information comes from mining engineers,
because of public incentives in order to work tin and tungsten deposits. In Spain, the
Instituto Geologico y Minero de España (IGME) is the entity who stores all the reports about
these investigations. In Portugal, the database SIORMINP, managed by the Laboratório
Nacional de Energia e Geologia (LNEG), available in internet, gives us information about
tin deposits, although it does not show elements about possible ancient works. We can
collect from this channel data about the geological context and the type of mineralisation
in each case. The negative point is the criterions used to detect and assess the interest of
the ore deposits are not comparable with the ones used in archaeological times.
The last group of documents is made up of archaeological works. The archaeological
path towards field work in mining studies has been slow. Archaeologists started studying
classical texts and objects from museums, and the first theories about the importance and
chronology of tin mining were built without field data. Joleaud gives us the first example
of such a work in 1929 8 : within two pages and a half, he maintains that tin had to be mined
in NW Iberia since the Bronze Age to make possible the production of all the bronze axes
known. Geological information is little by little integrated, for example by Serpa Pinto in
1933 in a synthesis about Portuguese mining activity during Bronze Age 9 or by Davies in
1935 in his Roman mines in Europe
suspiciously uncommon anywhere else
Africa
Kenya: Kilindini Harbour, which is a deep channel between Mombasa island and South Coast mainland, is a ria.
Asia
Sanriku Coast: North Japan, east coast of Honshū Island (main island). Sendai city, Miyagi Prefecture and Iwate Prefecture are included.
Coasts on western, southern sides of the Korean Peninsula: Rias formed by sea level rising after Ice Age.
Oceania
Papua New Guinea: Rias formed by eroded volcanic lava flow are found all around the town of Tufi at Cape Nelson, in Papua New Guinea’s Oro Province.
Australia: The east coast of Australia features several rias around Sydney, including Georges River, Port Hacking, and Sydney Harbour. There are many examples in Western Australia, including the Swan River around Perth and several rivers in the west Kimberley region.
New Zealand: Rias of various scales abound on the eastern shores of the upper North Island. On the west coast, in contrast, they are fewer but larger; Kaipara Harbour is the country’s largest, and the Hokianga Harbour, further north, is of historical significance to the native Māori people. The Marlborough Sounds at the northern tip of the South Island form a large network of rias.
North America
United States: Narragansett Bay, New York Harbor, Delaware Bay, Indian River Bay, the Chesapeake Bay, and Charleston Harbor are rias on the East Coast. Willapa Bay and Grays Harbor in Washington and San Francisco Bay in California on the West Coast are also rias.
Canada: Charlottetown Harbour, Prince Edward Island
South America
Argentina: Patagonia has the Deseado ria, on the coast of Santa Cruz Province, on the Atlantic Ocean.
https://pediaview.com/openpedia/Ria
Covering some 4,000 km2 of sounds, islands, and peninsulas, the Marlborough Sounds lie at the South Island’s north-easternmost point, between Tasman Bay in the west and Cloudy Bay in the south-east. The almost fractal coastline has 1/5 of the length of New Zealand’s coasts.
The steep, wooded hills and small quiet bays of the sounds are sparsely populated, as access is difficult. Many of the small settlements and isolated houses are only accessible by boat. The main large port is Picton on the mainland, at the head of Queen Charlotte Sound. It is at the northern terminus of the South Island’s main railway and state highway networks. The main small boat port is Waikawa which is one of New Zealand’s largest and provides a base for leisure sailors and vacationers.
The main sounds, other than Queen Charlotte Sound, are Pelorus Sound and Kenepuru Sound. Tory Channel is a major arm of Queen Charlotte Sound, and between them they isolate the hills of Arapaoa Island from the mainland. Other islands in the sounds include D’Urville Island.
Roman sandal found at Hadrian's Wall looks just like David Beckham's football boot
The shoe was discovered around a fortnight ago in the Severan ditch at the fort by Vindolanda archaeologists and will now go on permanent display. It is one of 420 shoes to have been found in the ditch, which was a Roman rubbish dump. Archaeologists have dated the shoe back to around 212AD and say it was been made from a single piece of leather.
You’d think the Roman fort of Vindolanda just south of Hadrian’s Wall was a footwear manufacturing concern rather than a military outpost with an attached a civilian settlement considering how many shoes have been found there. Literally thousands of shoes, their leather preserved in excellent condition by the waterlogged soil, have been unearthed at the fort and settlement over the decades. This season the excavation team has added another 350 shoes to the tally since digging began in April.
In 212, the Constitutio Antoniniana, issued by the emperor Caracalla, granted Roman citizenship to all the inhabitants of the empire, thus ending the second-class peregrini status. This made military diplomas largely redundant, and indeed the last known auxiliary diplomas date from AD 203.
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