Sunday, 2 September 2012
Monday, 27 August 2012
Compass experement with Basaltic andesite.
I recently experimented using a compass, firstly i placed a plastic wheelie bin well away from any metal objects, i then placed first a piece of rock taken from the great whinn sill at High force in upper teesdale on top of the bin. Then i approached the bin with the compass from about 3 metres, by the time i had placed the compass on top of the rock it had been deflected by 70-80 degrees.
Irepeated this proscess with similer sized pieces of rock my findings below.
Results
Whinn sill deflected 70-80 degrees ( High force)
Laverkiite deflected 20 degrees ( Staithes sea wall )
Coldberry ( Cleveland dyke ) 40-60 degrees
Stainton quarry Middlesbrough ( Cleveland dyke ) This i repeated 3 times 70- 180 degrees.
Irepeated this proscess with similer sized pieces of rock my findings below.
Results
Whinn sill deflected 70-80 degrees ( High force)
Laverkiite deflected 20 degrees ( Staithes sea wall )
Coldberry ( Cleveland dyke ) 40-60 degrees
Saturday, 25 August 2012
Auroch-Ox skull
I visited Dormans museum today with my daughters, we took the skull found by one of them at fairy dell south Midlesbrough, to compare with a 10.000 years plus skull they have on display said to have been found in Middlesbrough .
The skull my daughter found all them years ago still sits un viewed by the Cleveland public in my shed along side countless other ancient treasures , because of so called professional arrogance !
The image above shows the skull on display in a secure glass box in Dorman museum in Middlesbrough, titled as a short faced Ox? dating between 10 to 200,000 years bp
Above is one of the skulls found at fairy dell Middlesbrough by one of my daughters to the left being compared with the museum piece.
Sunday, 19 August 2012
Stainton gravel beds excavated at yet another location
The first image shows the approach down the deep beck valley side of maltby beck to the excavation.
The second image shows the early stages of the excavation, even at this stage i was in no doubt that i had found yet another continuation of the Stainton gravel beds.
The third image shows the gravel bed becoming more apparent, as are the deposits both above and below identical in make up and thickness as at my main stainton excavation at Stainton beck just short of a mile east
The seventh image shows a horse upper molar, these gravel beds ime told must be over 20.000 years old, yet ive also been told by professionals in the past that there were no horses in this area around that time !!! well ive found plenty.
The remaining images show the washed and dried bone found, the larger bone is a piece of a tibia but its to damaged to id.
Re: Tooth mineralization August 24, 2012 08:06PM |
Heath,
Teeth and bones start out as the mineral Hydroxylapatite (with some organic components too). During long burial in soil, some of the hydroxyl part (the "(OH)" in the chemical formula) can slowly get replaced by fluorine (F), and eventually the mineral part turns into the mineral Fluorapatite, which is a bit more resistant than the original Hydroxylapatite. There have been attempts to date old teeth and bones by the amount of fluorine they've absorbed, but I imagine there are so many variables involved that the results would be only a little bit superior to guesswork, although I haven't studied the method..
That's the reason that toothpaste contains "fluoride" - It's an attempt to speed up the replacement of the Hydroxylapatite in our teeth by Fluorapatite, making them more resistant to decay.
Depending on the soil chemistry in your area, other minerals could be entering the teeth too, like iron oxides, iron phosphates (vivianite, etc.), aluminium phosphates (variscite, etc.). The dark colour isn't necessarily from a mineral, however; it could be from the decomposition of the organic part of the tooth.
Cheers
Teeth and bones start out as the mineral Hydroxylapatite (with some organic components too). During long burial in soil, some of the hydroxyl part (the "(OH)" in the chemical formula) can slowly get replaced by fluorine (F), and eventually the mineral part turns into the mineral Fluorapatite, which is a bit more resistant than the original Hydroxylapatite. There have been attempts to date old teeth and bones by the amount of fluorine they've absorbed, but I imagine there are so many variables involved that the results would be only a little bit superior to guesswork, although I haven't studied the method..
That's the reason that toothpaste contains "fluoride" - It's an attempt to speed up the replacement of the Hydroxylapatite in our teeth by Fluorapatite, making them more resistant to decay.
Depending on the soil chemistry in your area, other minerals could be entering the teeth too, like iron oxides, iron phosphates (vivianite, etc.), aluminium phosphates (variscite, etc.). The dark colour isn't necessarily from a mineral, however; it could be from the decomposition of the organic part of the tooth.
Cheers
Thanks for that Petrov
Update on this excavation 26,8,2012
I excavated another metre in today although i did not discover as many fossils as usual, i did uncover this lower jaw piece, i also discovered a rich organic section below the tightly packed gravel bed.
The first image shows the sit before i started the second excavation.
Image two shows the upper jaw piece, i t was excavated about 2 metres into the packed gravel bed.
Image three shows the separate sequence of layers as at the main excavation at Stainton beck about a mile to the east.
Image four and five show the mandible after being washed.
Update on excavated fossils
This piece has coating a of many different small crystals the main stone is full of small Ammonites and coral among other unidentified pieces
The geological layers at this location are as follows-
Red - brown loamy friable almost stoneless clay.
Blue grey sandy clay containing organic material average thickness 100mm
Stainton gravel bed containing fossils and preserved mammall bones.
Mixture of sandy clay deposits and plastic almost stoneless red clay.
Location:Cleveland England
Maltby, Stockton-on-Tees, UK
Thursday, 16 August 2012
Ironstone hematite fossil dug from the Stainton gravel beds
Wednesday, 15 August 2012
Minerals recently found in upper Teesdale .
The two images above show a split rock found in the centre of an egg shaped geode, its coated in crystals.
The last image shows the inside of the rock found in the egg shaped geode.
Wednesday, 8 August 2012
Yorks magnetic curb stones
On a recent visit to York i found that the curb stones appear to be Whin stone, and ide bet they originate from one of the Cleveland Dyke quarries between Stainton and Cliff rigg. The image shows a rare earth magnet stuck to a curb stone not far from the Shambles,in York city centre.
The second image is the boothem area of york the curb stones tested here were also magnetic.
The second image is the boothem area of york the curb stones tested here were also magnetic.
Report on visit to teesdale to test the magnetic properties of both the Cleveland Dyke and Great Whinn Sill
http://youtu.be/srZsAaVGukA
http://youtu.be/9SIDRbMaOYY
The two links above show video's taken boy Roger Curry a good friend who is helping me into both the Magnetic qualities of the Cleveland Dyke and the Stainton newly discovered Gravel beds. The video's are not great but the conditions where very bad at one point we had a visit from a Tornado!
They basically show me and Roger testing both the Cleveland Dyke and the Great Whinn sill at Coldberry (Cleveland Dyke outcrop) and Great Whinn Sill at High force, Teesdale, we tested both with rare earth magnets and lesser powered magnets, our conclusion was this - The outcrop of Cleveland Dyke at Coldberry although magnetic was in no way as magnetic as the Stainton quarry whin stone ( Basaltic andesite) - The Great whinn sill at High force again although magnetic showed a far lower magnetic attraction than that of the Whin stone from the Stainton quarry samples tested over the last year.
I have now tested a fifty mile stretch of the Cleveland Dyke from Teesdale to the east coast and have found in all cases that the Stainton Quarry Whinnstone is by far the most magnetic.
For more info and images regarding my research into magnetic minerals please click the link below
The magnetic properties of the Cleveland dyke in t...
http://youtu.be/9SIDRbMaOYY
The two links above show video's taken boy Roger Curry a good friend who is helping me into both the Magnetic qualities of the Cleveland Dyke and the Stainton newly discovered Gravel beds. The video's are not great but the conditions where very bad at one point we had a visit from a Tornado!
They basically show me and Roger testing both the Cleveland Dyke and the Great Whinn sill at Coldberry (Cleveland Dyke outcrop) and Great Whinn Sill at High force, Teesdale, we tested both with rare earth magnets and lesser powered magnets, our conclusion was this - The outcrop of Cleveland Dyke at Coldberry although magnetic was in no way as magnetic as the Stainton quarry whin stone ( Basaltic andesite) - The Great whinn sill at High force again although magnetic showed a far lower magnetic attraction than that of the Whin stone from the Stainton quarry samples tested over the last year.
I have now tested a fifty mile stretch of the Cleveland Dyke from Teesdale to the east coast and have found in all cases that the Stainton Quarry Whinnstone is by far the most magnetic.
For more info and images regarding my research into magnetic minerals please click the link below
The magnetic properties of the Cleveland dyke in t...
Magnetic sea wall at Staithes
Mesolithic human tibia shaft excavated from the Stainton gravel beds
The tibia shaft shown in images 1 and 2 above i excavated from over two metres into the packed Stainton gravel beds.
This tibia shaft has today 13,9,12 been identified as an ancient human tibia shaft by anthropologists from a local university.
The tibia's below belonged to a long dead Viking's from the yorvik excavations at york
The Dorman museum in Middlesbrough now the only place i know of that could help, since Middlesbrough council removed all funding to Tees Archaeology, have been contacted and informed both of my discoveries ie the magnetic anomalies of the Stainton Quarry basaltic andesite, and the Stainton gravel beds and there rich fossil content, dated by Geologists who have visited as probably 12 - 16000ybp as yet ive had no response.
HISTORY OF A BECK: The Stainton gravel beds Locations of excavations of the Stainton gravel beds - Google Maps
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