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Car: Morris Minor 1000.
Year of manufacture: 1963.
Date of first registration in the UK: 14th May 1963.
Place of registration: Pembrokeshire.
Date of last MOT: 20th January 2010.
Mileage at last MOT: 19,036.
Date of last change of keeper: 9th April 2003.
Date taken: 7th July 2021.
Album: Carspotting 2021
We are all alike, but extremely different at the same time. It feels like everyone of us was born on another planet. So hard it might be sometimes to understand each other. Nevertheless, we try to do it as we live on the same planet named the Earth.
I feel like we all have 'a minor planet' of our own. It represents our view, experience, beliefs, prejudices and what not.What is important here is to be true to your planet.
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A 1960 Minor 1000 in 1:7 scale. Technic engine, suspension, transmission, steering, wipers, handbrake, adjustable seats.
Dans la constellation du Petit lion (Leo Minor), à 20 millions d'a.l. de la Terre, la galaxie spirale barrée NGC 3344 présente des anneaux et des bras spiraux modérés à lâches. Il existe à la fois un anneau intérieur et un anneau extérieur, les bras saillants rayonnant vers l’extérieur de l’anneau intérieur et la barre légèrement elliptique de l’intérieur. Cette image de Hubble est un composite réalisé avec sept filtres différents, couvrant des longueurs d’onde allant de l’ultraviolet à lumière visible et au proche infrarouge (cf. site Hubble).
Pour situer l'astre dans sa constellation :
www.flickr.com/photos/7208148@N02/48874028586/in/datepost...
The Aire and Calder Navigation is the canalised section of the Rivers Aire and Calder in West Yorkshire, England. The first improvements to the rivers above Knottingley were completed in 1704 when the Aire was made navigable to Leeds and the Calder to Wakefield, by the construction of 16 locks. Lock sizes were increased several times, as was the depth of water, to enable larger boats to use the system. The Aire below Haddlesey was bypassed by the opening of the Selby Canal in 1778. A canal from Knottingley to the new docks and new town at Goole provided a much shorter route to the River Ouse from 1826. The New Junction Canal was constructed in 1905, to link the system to the River Don Navigation, by then part of the Sheffield and South Yorkshire Navigation.
Steam tugs were introduced in 1831. In the 1860s, compartment boats were introduced, later called Tom Puddings, from which coal was unloaded into ships by large hydraulic hoists. This system enabled the canal to carry at its peak more than 1.5 million tons of coal per year, and was not abandoned until 1986. To handle trains of compartments, many of the locks were lengthened to 450 feet (140 m).
Although much of the upper reaches are now designated as leisure routes, there is still significant commercial traffic on the navigation. 300,000 tons were carried in 2007, although most of the traffic is now petroleum and gravel, rather than the coal which kept the navigation profitable for 150 years.
The Aire and Calder is a canalisation of the River Calder from Wakefield to Castleford, where it joins the branch from Leeds, which follows the River Aire. The Aire continues to flow eastwards to Bank Dole Junction, then continues in a north-easterly direction to Haddlesey, from where it follows a winding course to join the River Ouse at Airmyn. The section below Haddlesey is no longer part of the navigation, as a derelict lock blocks access to the lower river. Instead, the Selby Canal flows northwards from Haddlesey to the Ouse at Selby. Below Dole Bank Junction, the Knottingley and Goole Canal flows eastwards to join the Ouse at Goole. From just before Newbridge, where the modern A614 road crosses the waterway, this branch of the navigation runs parallel to the Dutch River, an artificial channel built in 1635 to alleviate flooding caused by Cornelius Vermuyden's original diversion of the River Don northwards to the River Aire in 1628.
The Aire and Calder still fulfils its original purpose of linking Leeds and Wakefield with York and the Humber (and thence the Trent), although the routes by which this is achieved have changed significantly. More recent canals now also make the Navigation a vital link in the English and Welsh connected inland waterway network. Beyond Leeds, the Leeds and Liverpool Canal carries boats over the Pennines. The Calder and Hebble Navigation, which connects to the Navigation at Wakefield, allows boats to reach the Huddersfield Broad and Narrow Canals, and the Rochdale Canal. The Selby Canal connects to the Ouse, from where boats can travel upstream to reach York, Boroughbridge and Ripon, or downstream to the River Derwent. Beyond Goole are the Humber and hence Hull, Immingham, and the North Sea. The Sheffield and South Yorkshire Navigation, which can be reached via the New Junction Canal, forms a link with Doncaster, Rotherham and Sheffield to the south west, and the tidal River Trent at Keadby to the east.
In the early 1600s, the River Aire was navigable to Knottingley, and boats carrying up to 30 tons traded on the river, which was tidal up to this point. The traders of Leeds were keen to have a navigable link to the town, to make easier the export of woollen cloth, but bills presented to Parliament in 1621 and 1625 had failed. William Pickering, who was mayor of Leeds, had made further attempts to obtain an act of Parliament for improvements to the river in 1679, again without success. As the 1600s drew to a close, a number of bills were passed for other rivers, and there was general support for river navigations. A bill was drawn up in 1698, with support from wool traders in Leeds and general merchants in Wakefield. John Hadley surveyed the Aire, and Samuel Shelton surveyed the Calder. Although the bill had a lot of support, it was opposed by the City of York, who feared that the River Ouse would be damaged by the scheme.
The parliamentary bill was hotly contested, and the House of Lords asked Trinity House to produce a report on the three rivers. This favoured the scheme, and in May 1699 the act of Parliament (10 Will. 3. c. 25) was granted. It named 18 undertakers, nine from the Corporation of Leeds, and nine "gentlemen of Wakefield", who would oversee the improvements to the River Aire (from the River Ouse at Airmyn via Castleford to Leeds) and the River Calder (from Castleford to Wakefield). The act gave them powers which included the creation of weirs bypassed by short "cuts" equipped with locks, the creation of a towpath, and the right to buy and demolish mills and weirs. John Hadley was engaged as the engineer immediately, and by 1704 the original work was completed, including 12 locks on the Aire between Haddesley and Leeds and 4 on the Calder. The locks were 58 to 60 feet (17.7 to 18.3 m) long by 14.5 to 15 feet (4.4 to 4.6 m) wide with 3.5 feet (1.1 m) depths over the sills.
Capital to fund the scheme had been raised separately by the Wakefield and Leeds committees. A complicated restructuring of the finances in 1721 fixed the nominal capital at £26,700. Regular dividends at 7 per cent were paid to the shareholders from 1718, and the navigation was leased to various groups, who would be responsible for collection of tolls and repairs. The lease rose from £800 in 1704 to £2,600 in 1729, when receipts from each of the previous five years had averaged £6,016. The early trade consisted mainly of woollen goods from Leeds, Wakefield, Halifax and Bradford, with wool and corn from Lincolnshire and East Anglia travelling in the opposite direction. By the 1720s there were also significant quantities of coal.
On 10 May 2021, an articulated lorry crashed off a bridge from the M62 and into the navigation. The tractor unit landed on the bank and the driver suffered minor injuries, while the trailer floated away
Dreamers by Cica Ghost
In a surreal world canopied by a magical sky, sixteen figures look upward to dream. This is one of their dreams brought back to the kitchen table.
maps.secondlife.com/secondlife/LEA24/91/45/28
Music stream: 94.23.51.96:8000
en.wikipedia.org/wiki/Morris_Minor_(1928)
Haynes International Motor Museum, Breakfast Club, Sunday 6th October 2019.
Car: Morris Minor 1000.
Date of first registration: 29th June 1965.
Registration region: Pembrokeshire.
Latest recorded mileage: 36,372 (MOT 24th November 2017).
Last V5 issued: 9th May 2012.
Date taken: 17th August 2020.
Album: Carspotting
all comes down to the last hours before falling apart.. not much sleep these days, but always motivated regardless. #200 finally, now its a significant reason to purchase pro again in April ;)
Canon 5D Mark II,
35mm 1.4L
Car: Morris Minor 1000.
Date of first registration: 29th June 1965.
Registration region: Pembrokeshire.
Latest recorded mileage: 36,372 (MOT 24th November 2017).
Last V5 issued: 9th May 2012.
Date taken: 17th August 2020.
Album: Carspotting
The Minor had a production run from 1948-71 so they were produced by Morris, BMC and latterly British Leyland. The Traveller was produced from 1953 with this one rolling of the production line in 1968. Desertmartin Parish Church Garden Fete & Vintage Rally 2025.
Vehicle: Morris Minor 1000 Traveller.
Date of first registration: 1st January 1963.
Registration region: Hertfordshire.
Latest recorded mileage: 40,858 (MOT 11th December 2018).
Date taken: 9th April 2019.
Album: Street Spots
Periwinkle (Vinca minor) is a creeping ground cover that has spread from gardens. It is so common that it is occasionally mistaken for a wildflower. The five petals create a pinwheel effect with a star outlined in the center. The evergreen leaves are glossy and appear in opposite pairs. (Source: "A Field Guide to Wildflowers of Northeastern and North-central North America" by Roger Tory Peterson and Margaret McKenny)
1970 Morris Minor
Production of this car was winding down when this car was manufactured in 1970
This car had a long production run from 1948 until 1971
With just small changes to the design along the 23 Year journey of production.
Looking immaculate in the early spring sunshine. There's a story about it here: www.walsham-le-willows.org/morris-minor-fundraising-tour-...
That article mentions it having a 948cc engine, but DVLA says it's just 803cc. Maybe it's been upgraded to make it a little more driveable in modern traffic conditions?
I revisited this magnificent nature reserve today 10th August 2018, many visitors to our city miss its glorious offerings, thinking all we have to offer is the beach front at the main boulevard , its a pity as this reserve is a short drive from the main tourist area and has its own charm, attraction and wealth of nature on offer, I love it .
Donmouth Local Nature Reserve is a beach site in the historic Old Aberdeen part of the City where the River Don meets the sea.
A great place to see seals and a range of interesting birds. The beach area has changed over time as the river has changed its course. There are lots of interesting plants in the dunes and beach area. Bird hide is an excellent shelter from which to watch the wildlife. The paths run across King Street to the Brig 'o Balgownie., the original bridge in to the City from the North, then down the other side of the river to the sea.
The site was designated a Local Nature Reserve in 1992
Paths are good although wheelchair access to the beach would be difficult as the boardwalk can get covered with sand.
There is plenty of free car parking on the Beach Esplanade and at the car park in Donmouth Road. There are cycle racks on Beach Esplanade
Bridge Of Don has five spans of dressed granite, and rounded cutwaters that carry up to road level to form pedestrian refuges. The spans are 75 feet (23 m), with a rise of 25 feet (7.6 m).
It was widened in 1958-59, from 24 feet (7.3 m), to 66 feet (20 m) by the construction of a new concrete bridge adjacent to the old one.
It now carries four lanes of the A956 road, and is the last bridge on the River Don before it meets the sea. The bridge is just downstream from a substantial island in the river. Around the area of the bridge is the Donmouth Local Nature Reserve, designated as a LNR in 1992.
Near to the bridge are a number of World War II era coastal defences, including a pill box.
Mudflats
Mudflats are formed when fine particles carried downstream by the river are deposited as it slows down before entering the sea, and to a lesser extent by fine particles washed in by the tide. The sand spit at the mouth of the Don provides shelter from the wind and waves allowing this material to build up. The mud flats are a very rich and fertile environment. Despite their rather barren appearance they support a surprisingly diverse invertebrate fauna which includes; worms, molluscs and crustacea. These invertebrates are vitally important to wildfowl and wading birds within the estuary.
Salt marsh
Along the upper shore of the south bank saltmarsh has developed. This habitat would once have been much more extensive prior to the tipping of domestic and other refuse in the area and the formation in 1727 of an artificial embankment to prevent flooding of the river into the Links. This habitat is now reduced to a narrow strip of vegetation along the river margins upstream from the Powis Burn.
The species composition of the salt marsh varies according to the salinity of the water i.e. the proximity to the sea. Close to the Powis Burn this habitat is dominated by reed sweet-grass (Glyceria maxima) with reed canary-grass (Phalaris arundinacea), sea club-rush (Scirpus maritimus), spike-rush (Eleocharis palustris), hemlock water-dropwort (Oenanthe crocata) and common scurvygrass (Chochlearia officinalis).
Further inland reed sweet-grass continues to dominate but hemlock water-dropwort is more abundant with meadowsweet (Filipendula ulmaria) and valarian (Valariana officinalis),
Sand dunes
Sand dunes are found in the more exposed parts of the estuary at the river mouth. Again, this habitat was once much more extensive in this locality with dune grasslands stretching from Aberdeen Beach inland as far as King Street, southwards from the estuary of the Dee, northwards to the Sands of Forvie and beyond. Many of the dunes formed part of Seaton Tip, and following tipping the area was grassed over. Other areas have been formally landscaped to form golf courses or planted with native trees in 2010 to create a new woodland area.
Some remnants of the natural dune flora can be seen in the 'roughs' on the Kings Links golf course and near the mouth of the river.
Above the high water mark, fore dunes with thick clumps of the pioneer grass species including sea lyme grass (Elymus arenarius) and marram grass (Ammophila arenaria) occur. Few other species are able to cope with the shifting sand. The largest area of these young dunes is to the north and west of the headland. Further inland where the dunes are sheltered from the actions of the wind and waves, and soils are more developed, more stable dunes are present supporting a more diverse grassland habitat.
Strand line plants which are able to tolerate occasional coverage by sea water include sea rocket (Cakile maritima), frosted orache (Atriplex laciniata), sea sandwort (Honkenya peploides) and knotgrass (Polygonum aviculare). Bur-reed (Sparganium sp.) has been recorded; presumably washed down by the river.
Marram grass (Ammophila arenaria) and sea lyme grass (Elymus arenarius) dominate the fore dunes. The latter species is not native to this area but appeared in 1802. It is thought to have been unintentionally introduced into the area by fishing boats. For a number of years it remained uncommon but from 1870 onwards it spread rapidly along the coastline (Marren, 1982).
In the more stable dunes red fescue (Festuca rubra), sand sedge (Carex arenaria), yellow rattle (Rhinanthus minor), wild pansy (Viola tricolour), harebell (Campanula rotundifolia), bird's-foot-trefoil (Lotus corniculatus) and lesser meadow-rue (Thalictrum minus) are abundant. Small amounts of kidney vetch (Anthyllis vulneraria), valerian (Valeriana officinalis) and spring vetch (Vicia lathyroides) are present.
Scattered willows (Salix sp.) and sycamore (Acer pseudoplantanus) have seeded into this area. Gorse (Ulex europaeus) scrub has colonised the dunes in some areas and appears to be spreading.
Scrub
This habitat is almost entirely artificial with only the gorse scrub on the inner dunes being a semi-natural habitat. Alder and willow were planted along the south bank of the river in about 1970 and these shrubs are now generally well established. Further shrub planting on the south bank was carried out in 1990.
Willow (Salix sp.) and alder (Alnus glutinosa) were planted in the 1970's along the south bank of the River Don eastwards of the Bridge of Don. The trees to the west of this strip are doing considerably better than those to the east. More recent planting was carried out in 1990 with hawthorn (Crataegus monogyna), blackthorn (Prunus spinosa) elder (Sambucus nigra), goat willow (Salix caprea) and alder.
Underneath the scrub neutral grassland is present with cocksfoot (Dactylis glomerata), false oat-grass (Arrhenatherum elatius), cow parsley (Anthriscus sylvestris), sweet cicely (Myrrhis odorata), hedge woundwort (Stachys sylvatica) and hedge bindweed (Calystegia sepium).
Grassland
Much of the grassland within the reserve is formed on imported soil and is intensively managed. This includes grassland on the north and south sides of the Esplanade. Daffodils are present in the grassland on the north side of the road. On the north bank to the east of the Bridge of Don is rank grassland on a steep south-facing slope. This is unmanaged and contains some patches of scrub.
Rough grassland is present on the headland. This area has been modified by tipping, with rubble to the east and with grass cuttings to the west. The grassland contains a mixture of neutral grassland, dune grassland, ruderal, and introduced garden species. This area attracts flocks of seed eating birds in late summer and autumn.
Improved grassland is present on the headland and along the south bank of the estuary downstream from the bridge of Don. Much of this vegetation has developed on imported soil and contains a high proportion of ruderal species and garden escapes. On the headland, broadleaved dock (Rumex obtusifolius), nettle (Urtica dioica), coltsfoot (Tussilago farfara), spear thistle (Cirsium vulgare), cow parsley (Anthriscus sylvestris), hemlock (Conium maculatum) and hogweed (Heracleum sphondylium) are abundant. Sweet cicely (Chaerophyllum bulbosum) is widespread and in late summer fills the air with the scent of aniseed.
To the south of the Esplanade the grassland is managed with an annual cut.. The grassland does flood to form pools. Early in the year cuckoo flower (Cardamine pratensis) is common, meadow foxtail (Alopecuris pratensis)is known to occur around the margins of these pools.
Woodland
Semi-mature woodland is present on the steep sided south bank of the river upstream from the Bridge of Don. Most of this woodland has been planted in the mid 1930's though some older oak and elm trees are present. These may be relicts of former woodland cover. The woodland in the reserve is part of a strip of woodland along the River Don corridor which continues upstream from the Brig 'o' Balgownie.
Woodland is present on the south bank upstream from the Bridge of Don.
Much of the woodland consists of even aged stands with willow (Salix sp.), sycamore (Acer pseudoplatanus), ash (Fraxinus excelsior), beech (Fagus sylvatica) and alder (AInus glutinosa). At the top of the slope mature oak (Quercus sp.) and elm (Ulmus glabra) are present. The ground flora contains tufted hair-grass (Deschampsia caespitosa), red campion (Silene dioica), ramsons (Allium ursinum) and lady fern (Athyrium felix-femina) .In a few areas dense shading is caused by the trees and in these areas the ground flora is poor.
On the north bank scattered trees are present, mainly willow and sycamore with some scrub.