Una inquadratura del piccolo grande porticciolo -…
Lyon (69) 27 janvier 2024. Funiculaire montant à F…
Man sollte seine Antennen immer richtig einstellen…
Du côté de Valencienne . HWW.
HWW: Ecke
Le Dahu DxO 1080
WALL
Il 'caruggiu' che porta al porticciolo di Camogli
Entre le 12ème et le 4ème arrondissements
Elle est à moi..!
Du coté de l'Andalousie en Espagne.
Château de Saint Montant.
HFF Jurong Singapore 1980
HFF et agréable fin de semaine.
Camogli : riflessi nel porto -
It blooms!
hammock for a good rest
Colori e riflessi nel porto di Camogli
Du côté de Valencienne 02.
Netteté visuelle au maximale
SSC -Müll-
Souriez... !
L'abbatiale du Montglonne.
Entre le 11ème et le 12ème arrondissement
Art : lien entre passé et présent
Dans le panneau... solaire
Old water-wheel.
Stencil at Alfama.
Tiles panel.
Tourism Office, in typical local architecture.
Piggy bank for tips.
Camogli : poco spazio per costruire : le case hann…
Très peureuse..!
Coming from Lisbon.
Painting on abandoned house.
Dante Museum.
Vincent
Basilica of Mafra's Convent (18th century).
Royal Building of Mafra (18th century).
Weg nach Puerto Calero
April 22nd, Earth Day
Général vendéen BONCHAMPS.
la lune
Quanta attrezzatura serve per catturare un po' di…
HBM Belton Grantham Lincolnshire 15th April 2024
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46 visits
HWW Kimberley Northern Cape South Africa 2nd June 1982
It's difficult to capture the depth of the "Big Hole" in Kimberley but the height of the buildings give an idea of the scale. It's a real vertical wall of rock.
Kimberlite, an ultramafic igneous rock and a rare variant of peridotite, is most commonly known to be the main host matrix for diamonds. It is named after Kimberley where diamonds were mined from this hole.
Kimberlite occurs in the Earth's crust in vertical structures known as kimberlite pipes, as well as igneous dykes and can also occur as horizontal sills. The consensus on kimberlites is that they are formed deep within the mantle, hence at high temperatures and pressures.
HWW to everyone. Have a great day!
Kimberlite, an ultramafic igneous rock and a rare variant of peridotite, is most commonly known to be the main host matrix for diamonds. It is named after Kimberley where diamonds were mined from this hole.
Kimberlite occurs in the Earth's crust in vertical structures known as kimberlite pipes, as well as igneous dykes and can also occur as horizontal sills. The consensus on kimberlites is that they are formed deep within the mantle, hence at high temperatures and pressures.
HWW to everyone. Have a great day!
Nouchetdu38, Eva Lewitus, Ulrich John, Don Sutherland and 8 other people have particularly liked this photo
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HWW, enjoy the day. Herb
Thank you for the interesting information Pete. Peridotite is the primary source of the peridot gemstone also I understand. It must have been a fascinating visit.
HWW
en.wikipedia.org/wiki/Big_Hole
en.wikipedia.org/wiki/Super_Pit_gold_mine
Or this smaller one south of Cobar, Australia. www.ipernity.com/doc/grahamh/24301253
Loose_Grip/Pete club has replied to GrahamH clubGrahamH club has replied to Loose_Grip/Pete clubHWW Pete
HFF & Best wishes
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