Testing - Revision history

Cornel at 23:16, 6 April 2025

2025-04-06T23:16:01Z

← Older revision		Revision as of 23:16, 6 April 2025
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	{\| class=wikitable align=right border="3"		{\| class=wikitable align=right border="3"
			! colspan="2" style="background: #FFF0D9;" \| <big>''' Casa Greceanu '''</big>
	! colspan="2" style="background: #~~ffdead~~;" \| <big>''' Casa Greceanu '''</big>
	[[File:Casa+Greceanu+Eduard+Pesky_1885+4C.jpg\|300px\|thumb\|center\|]]		[[File:Casa+Greceanu+Eduard+Pesky_1885+4C.jpg\|300px\|thumb\|center\|]]
	'''Adresa''': Calea Victoriei Nr. 30		'''Adresa''': Calea Victoriei Nr. 30
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	{\| class=wikitable align=right border="3"		{\| class=wikitable align=right border="3"

	! colspan="2" style="background: #~~006699~~;" \| <big>''' Casa Greceanu '''</big>		! colspan="2" style="background: #BFE2FF;" \| <big>''' Casa Greceanu '''</big>
	[[File:Casa+Greceanu+Eduard+Pesky_1885+4C.jpg\|300px\|thumb\|center\|]]		[[File:Casa+Greceanu+Eduard+Pesky_1885+4C.jpg\|300px\|thumb\|center\|]]
	'''Adresa''': Calea Victoriei Nr. 30		'''Adresa''': Calea Victoriei Nr. 30

Cornel at 23:10, 6 April 2025

2025-04-06T23:10:28Z

← Older revision		Revision as of 23:10, 6 April 2025
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	{\| class=wikitable align=right border="3"		{\| class=wikitable align=right border="3"

	\|scope="col" align=center\| <big>'''Calea Victoriei'''</big>		\|scope="col" align=center\| <big>'''Calea Victoriei'''</big>


	[[File:Calea_Victoriei_9_Magazinul_Sigmud_Prager_1940.jpg\|300px\|thumb\|center\|]]		[[File:Calea_Victoriei_9_Magazinul_Sigmud_Prager_1940.jpg\|300px\|thumb\|center\|]]

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	The 1940 earthquake registered a magnitude of 7.7 on the moment magnitude scale, being the strongest earthquake recorded in the 20th century in Romania.[7] Its epicenter lay in the Vrancea zone at a depth of about 133 km. The area of maximum intensity for this earthquake was 80,000 km2[4] and macroseismic effects were felt over an area of more than 2,000,000 km2.[3] Effects were reported to the north as far away as Leningrad, over 1,300 km away,[8] with estimated seismic intensities of IV–V (MCS degrees), to the south, as far as Greece, to the east, up to the Kharkov–Moscow line, with estimated intensities of V–VI (MCS degrees), in the west, as far as Belgrade, Budapest and Warsaw.		The 1940 earthquake registered a magnitude of 7.7 on the moment magnitude scale, being the strongest earthquake recorded in the 20th century in Romania.[7] Its epicenter lay in the Vrancea zone at a depth of about 133 km. The area of maximum intensity for this earthquake was 80,000 km2[4] and macroseismic effects were felt over an area of more than 2,000,000 km2.[3] Effects were reported to the north as far away as Leningrad, over 1,300 km away,[8] with estimated seismic intensities of IV–V (MCS degrees), to the south, as far as Greece, to the east, up to the Kharkov–Moscow line, with estimated intensities of V–VI (MCS degrees), in the west, as far as Belgrade, Budapest and Warsaw.
	Vrancea lies within the Carpathian Mountains, which were formed as part of the Alpine Orogeny. The convergence across this zone stopped about 20 million years ago, but the area remains seismically active. The earthquakes have reverse fault focal mechanisms and define a southwest–northeast trending zone about 70 km long by 30 km across. The depth range of the earthquakes extends from 60 km down to about 200 km. Seismic tomography studies show that the area is underlain by a body with a high seismic velocity. There are two models available to explain these observations, a detached subducting slab and delamination of the lower crust. The near vertical geometry of the high-velocity body combined with the focal mechanisms are consistent with extension along the body. Combined with the lack of a clear planar zone of seismicity that would be expected for a subducting slab, this is consistent with some form of delamination.[9]


			Vrancea lies within the Carpathian Mountains, which were formed as part of the Alpine Orogeny. The convergence across this zone stopped about 20 million years ago, but the area remains seismically active. The earthquakes have reverse fault focal mechanisms and define a southwest–northeast trending zone about 70 km long by 30 km across. The depth range of the earthquakes extends from 60 km down to about 200 km. Seismic tomography studies show that the area is underlain by a body with a high seismic velocity. There are two models available to explain these observations, a detached subducting slab and delamination of the lower crust. The near vertical geometry of the high-velocity body combined with the focal mechanisms are consistent with extension along the body. Combined with the lack of a clear planar zone of seismicity that would be expected for a subducting slab, this is consistent with some form of delamination.
	~~<td style="background~~-~~color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h2 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf~~. ~~Ionica </h2></td>~~


	<td style="background-color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h1 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf. Ionica </h1></td>		<td style="background-color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h1 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf. Ionica </h1></td>

			{\| style="float: right; border: 1px solid #BBB; margin: .46em 0 0 .2em;"
			\|- style="font-size: 86%;"
			\| valign="top" \|[[File:DuraEuropos-TempleOfBel.jpg\|180px]]<!--
			--><br /> Temple of [[Bel (mythology)\|Bel]] (floating).
			\|}
			{\| style="float: right; border: 1px solid #BBB; margin: .46em 0 0 .2em;"
			\|- style="font-size: 86%;"
			\| valign="top" \|[[File:DuraEuropos-TempleOfBel.jpg\|180px]]<!--
			--><br /> Temple of [[Bel (mythology)\|Bel]] (floating).
			\|}
			{\| style="float: right; border: 1px solid #BBB; margin: .46em 0 0 .2em;"
			\|- style="font-size: 86%;"
			\| valign="top" \|[[File:DuraEuropos-TempleOfBel.jpg\|180px]]<!--
			--><br /> Temple of [[Bel (mythology)\|Bel]] (floating).
			\|}


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			{\| class=wikitable align=right border="3"

			! colspan="2" style="background: #ffdead;" \| <big>''' Casa Greceanu '''</big>
			[[File:Casa+Greceanu+Eduard+Pesky_1885+4C.jpg\|300px\|thumb\|center\|]]
			'''Adresa''': Calea Victoriei Nr. 30

			'''Adresa ''': Podul Mogosoaiei

			'''Ani in existenta''': Sec. XVIII-1944

			[https://maps.app.goo.gl/BzbjNK1jozZHnAXS7 '''Google Maps''']

			'''In cladire au functionat''': Casa Coconilor

			'''Autor''': Cornel D. [[File:Cd1.png\|16px\| ]]
			[[Calea Victoriei]] [[Imobile\|Palate/Imobile]]
			\|}








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	{\| class=wikitable align=right border="3"		{\| class=wikitable align=right border="3"

	! colspan="2" style="background: #~~ffdead~~;" \| <big>''' Casa Greceanu '''</big>		! colspan="2" style="background: #006699;" \| <big>''' Casa Greceanu '''</big>
	[[File:Casa+Greceanu+Eduard+Pesky_1885+4C.jpg\|300px\|thumb\|center\|]]		[[File:Casa+Greceanu+Eduard+Pesky_1885+4C.jpg\|300px\|thumb\|center\|]]
	'''Adresa''': Calea Victoriei Nr. 30		'''Adresa''': Calea Victoriei Nr. 30

Cornel at 22:36, 6 April 2025

2025-04-06T22:36:24Z

← Older revision		Revision as of 22:36, 6 April 2025
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	<td style="background-color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h1 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf. Ionica </h1></td>		<td style="background-color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h1 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf. Ionica </h1></td>




























			{\| class=wikitable align=right border="3"

			! colspan="2" style="background: #ffdead;" \| <big>''' Casa Greceanu '''</big>
			[[File:Casa+Greceanu+Eduard+Pesky_1885+4C.jpg\|300px\|thumb\|center\|]]
			'''Adresa''': Calea Victoriei Nr. 30

			'''Adresa ''': Podul Mogosoaiei

			'''Ani in existenta''': Sec. XVIII-1944

			[https://maps.app.goo.gl/BzbjNK1jozZHnAXS7 '''Google Maps''']

			'''In cladire au functionat''': Casa Coconilor

			'''Autor''': Cornel D. [[File:Cd1.png\|16px\| ]]
			[[Calea Victoriei]] [[Imobile\|Palate/Imobile]]
			\|}

Cornel at 02:54, 20 March 2025

2025-03-20T02:54:12Z

← Older revision		Revision as of 02:54, 20 March 2025
Line 38:		Line 38:

	<td style="background-color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h2 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf. Ionica </h2></td>		<td style="background-color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h2 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf. Ionica </h2></td>


			<td style="background-color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h1 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf. Ionica </h1></td>

Cornel at 22:53, 18 March 2025

2025-03-18T22:53:18Z

← Older revision		Revision as of 22:53, 18 March 2025
Line 34:		Line 34:
	The 1940 earthquake registered a magnitude of 7.7 on the moment magnitude scale, being the strongest earthquake recorded in the 20th century in Romania.[7] Its epicenter lay in the Vrancea zone at a depth of about 133 km. The area of maximum intensity for this earthquake was 80,000 km2[4] and macroseismic effects were felt over an area of more than 2,000,000 km2.[3] Effects were reported to the north as far away as Leningrad, over 1,300 km away,[8] with estimated seismic intensities of IV–V (MCS degrees), to the south, as far as Greece, to the east, up to the Kharkov–Moscow line, with estimated intensities of V–VI (MCS degrees), in the west, as far as Belgrade, Budapest and Warsaw.		The 1940 earthquake registered a magnitude of 7.7 on the moment magnitude scale, being the strongest earthquake recorded in the 20th century in Romania.[7] Its epicenter lay in the Vrancea zone at a depth of about 133 km. The area of maximum intensity for this earthquake was 80,000 km2[4] and macroseismic effects were felt over an area of more than 2,000,000 km2.[3] Effects were reported to the north as far away as Leningrad, over 1,300 km away,[8] with estimated seismic intensities of IV–V (MCS degrees), to the south, as far as Greece, to the east, up to the Kharkov–Moscow line, with estimated intensities of V–VI (MCS degrees), in the west, as far as Belgrade, Budapest and Warsaw.
	Vrancea lies within the Carpathian Mountains, which were formed as part of the Alpine Orogeny. The convergence across this zone stopped about 20 million years ago, but the area remains seismically active. The earthquakes have reverse fault focal mechanisms and define a southwest–northeast trending zone about 70 km long by 30 km across. The depth range of the earthquakes extends from 60 km down to about 200 km. Seismic tomography studies show that the area is underlain by a body with a high seismic velocity. There are two models available to explain these observations, a detached subducting slab and delamination of the lower crust. The near vertical geometry of the high-velocity body combined with the focal mechanisms are consistent with extension along the body. Combined with the lack of a clear planar zone of seismicity that would be expected for a subducting slab, this is consistent with some form of delamination.[9]		Vrancea lies within the Carpathian Mountains, which were formed as part of the Alpine Orogeny. The convergence across this zone stopped about 20 million years ago, but the area remains seismically active. The earthquakes have reverse fault focal mechanisms and define a southwest–northeast trending zone about 70 km long by 30 km across. The depth range of the earthquakes extends from 60 km down to about 200 km. Seismic tomography studies show that the area is underlain by a body with a high seismic velocity. There are two models available to explain these observations, a detached subducting slab and delamination of the lower crust. The near vertical geometry of the high-velocity body combined with the focal mechanisms are consistent with extension along the body. Combined with the lack of a clear planar zone of seismicity that would be expected for a subducting slab, this is consistent with some form of delamination.[9]



			<td style="background-color: #e1e1e1;" style="font-family:Papyrus;" style="font-size:x-large;" style="font-weight:bold;"><h2 style="text-align: left;" style="font-family: papyrus;"> Biserici Disparute - Biserica Sf. Ionica </h2></td>

Cornel at 00:37, 10 March 2025

2025-03-10T00:37:47Z

← Older revision		Revision as of 00:37, 10 March 2025
Line 34:		Line 34:
	The 1940 earthquake registered a magnitude of 7.7 on the moment magnitude scale, being the strongest earthquake recorded in the 20th century in Romania.[7] Its epicenter lay in the Vrancea zone at a depth of about 133 km. The area of maximum intensity for this earthquake was 80,000 km2[4] and macroseismic effects were felt over an area of more than 2,000,000 km2.[3] Effects were reported to the north as far away as Leningrad, over 1,300 km away,[8] with estimated seismic intensities of IV–V (MCS degrees), to the south, as far as Greece, to the east, up to the Kharkov–Moscow line, with estimated intensities of V–VI (MCS degrees), in the west, as far as Belgrade, Budapest and Warsaw.		The 1940 earthquake registered a magnitude of 7.7 on the moment magnitude scale, being the strongest earthquake recorded in the 20th century in Romania.[7] Its epicenter lay in the Vrancea zone at a depth of about 133 km. The area of maximum intensity for this earthquake was 80,000 km2[4] and macroseismic effects were felt over an area of more than 2,000,000 km2.[3] Effects were reported to the north as far away as Leningrad, over 1,300 km away,[8] with estimated seismic intensities of IV–V (MCS degrees), to the south, as far as Greece, to the east, up to the Kharkov–Moscow line, with estimated intensities of V–VI (MCS degrees), in the west, as far as Belgrade, Budapest and Warsaw.
	Vrancea lies within the Carpathian Mountains, which were formed as part of the Alpine Orogeny. The convergence across this zone stopped about 20 million years ago, but the area remains seismically active. The earthquakes have reverse fault focal mechanisms and define a southwest–northeast trending zone about 70 km long by 30 km across. The depth range of the earthquakes extends from 60 km down to about 200 km. Seismic tomography studies show that the area is underlain by a body with a high seismic velocity. There are two models available to explain these observations, a detached subducting slab and delamination of the lower crust. The near vertical geometry of the high-velocity body combined with the focal mechanisms are consistent with extension along the body. Combined with the lack of a clear planar zone of seismicity that would be expected for a subducting slab, this is consistent with some form of delamination.[9]		Vrancea lies within the Carpathian Mountains, which were formed as part of the Alpine Orogeny. The convergence across this zone stopped about 20 million years ago, but the area remains seismically active. The earthquakes have reverse fault focal mechanisms and define a southwest–northeast trending zone about 70 km long by 30 km across. The depth range of the earthquakes extends from 60 km down to about 200 km. Seismic tomography studies show that the area is underlain by a body with a high seismic velocity. There are two models available to explain these observations, a detached subducting slab and delamination of the lower crust. The near vertical geometry of the high-velocity body combined with the focal mechanisms are consistent with extension along the body. Combined with the lack of a clear planar zone of seismicity that would be expected for a subducting slab, this is consistent with some form of delamination.[9]








































	~~{\| class="wikitable" style="width: 100%;" style="margin: auto;" style="text-align: left;" align=right~~
	~~\| style="width: 50%; style="font-style: italic; color: DarkSlateGray;" \|~~
	~~<pre "color: DarkSlateGray"> </pre>~~
	~~<gallery>~~
	~~File:Calea_Victoriei_9_Magazinul_Sigmud_Prager_1940.jpg~~
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	\|}

Cornel at 04:05, 9 March 2025

2025-03-09T04:05:35Z

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 [[File:Calea_Victoriei_9_Magazinul_Sigmud_Prager_1940.jpg|300px|thumb|center|]]
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 The 1940 earthquake registered a magnitude of 7.7 on the moment magnitude scale, being the strongest earthquake recorded in the 20th century in Romania.[7] Its epicenter lay in the Vrancea zone at a depth of about 133 km. The area of maximum intensity for this earthquake was 80,000 km2[4] and macroseismic effects were felt over an area of more than 2,000,000 km2.[3] Effects were reported to the north as far away as Leningrad, over 1,300 km away,[8] with estimated seismic intensities of IV–V (MCS degrees), to the south, as far as Greece, to the east, up to the Kharkov–Moscow line, with estimated intensities of V–VI (MCS degrees), in the west, as far as Belgrade, Budapest and Warsaw.
 Vrancea lies within the Carpathian Mountains, which were formed as part of the Alpine Orogeny. The convergence across this zone stopped about 20 million years ago, but the area remains seismically active. The earthquakes have reverse fault focal mechanisms and define a southwest–northeast trending zone about 70 km long by 30 km across. The depth range of the earthquakes extends from 60 km down to about 200 km. Seismic tomography studies show that the area is underlain by a body with a high seismic velocity. There are two models available to explain these observations, a detached subducting slab and delamination of the lower crust. The near vertical geometry of the high-velocity body combined with the focal mechanisms are consistent with extension along the body. Combined with the lack of a clear planar zone of seismicity that would be expected for a subducting slab, this is consistent with some form of delamination.[9]
 {| class="wikitable" style="width: 100%;" style="margin: auto;" style="text-align: left;"  align=right

Cornel at 03:24, 9 March 2025

2025-03-09T03:24:17Z

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Cornel: Created page with " {| class="wikitable" style="width: 100%;" style="margin: auto;" style="text-align: left;" align=right | style="width: 50%; style="font-style: italic; color: DarkSlateGray;" |

File:Calea_Victoriei_9_Magazinul_Sigmud_Prager_1940.jpg

|} {| class=wikitable align=right | AA || BB |- | CD || EF |}"

2025-03-09T03:17:16Z

Created page with " {| class="wikitable" style="width: 100%;" style="margin: auto;" style="text-align: left;" align=right | style="width: 50%; style="font-style: italic; color: DarkSlateGray;" | <pre "color: DarkSlateGray"> </pre> <gallery> File:Calea_Victoriei_9_Magazinul_Sigmud_Prager_1940.jpg </gallery> <pre "color: DarkSlateGray"> </pre> |} {| class=wikitable align=right | AA || BB |- | CD || EF |}"

New page

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File:Calea_Victoriei_9_Magazinul_Sigmud_Prager_1940.jpg
</gallery>
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|}

{| class=wikitable align=right
| AA || BB
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| CD || EF
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