Среќен Роденден

African Plate spin­ning

African Plate spin­ning

Char­lotte par­tic­i­pates in en­ter­tain­ment

Char­lotte par­tic­i­pates in en­ter­tain­ment

World on Your Plate: North African

World on Your Plate: North African

On Sat­ur­day 31 July Al­ge­ri­an and Mo­roc­can cui­sine was a de­light for the sens­es in the Mu­se­um Atri­um — co­rian­der, cumin, saf­fron, mar­jo­ram and onion scents min­gled with the pun­gen­cy of olive oil to tan­ta­lise vis­i­tors taste­buds as they sipped mint tea and sam­pled the best of North African cui­sine. Chef Makh Benyet­tou, of Sahaa Restau­rant, demon­strat­ed his fab­u­lous 'fig cous­cous' and 'cous­cous royale' dish­es. Belly dancer, Can­dice Fran­k­land, en­thralled vis­i­tors with her grace­ful move­ments to the Ara­bi­an beats of North Africa. See Makh's recipe for fig cous­cous on the Kai to Pie blog blog.​aucklandmuseum.​com For more info about the Kai to Pie ex­hi­bi­tion check out www.​aucklandmuseum.​com .

On Sat­ur­day 31 July Al­ge­ri­an and Mo­roc­can cui­sine was a de­light for the sens­es in the Mu­se­um Atri­um — co­rian­der, cumin, saf­fron, mar­jo­ram and onion scents min­gled with the pun­gen­cy of olive oil to tan­ta­lise vis­i­tors taste­buds as they sipped mint tea and sam­pled the best of North African cui­sine. Chef Makh Benyet­tou, of Sahaa Restau­rant, demon­strat­ed his fab­u­lous 'fig cous­cous' and 'cous­cous royale' dish­es. Belly dancer, Can­dice Fran­k­land, en­thralled vis­i­tors with her grace­ful move­ments to the Ara­bi­an beats of North Africa. See Makh's recipe for fig cous­cous on the Kai to Pie blog blog.​aucklandmuseum.​com For more info about the Kai to Pie ex­hi­bi­tion check out www.​aucklandmuseum.​com .

SAGID ALI DESTA PLATE SPIN­NING COM­E­DY ACT.(AFRICAN CIR­CUS AC­RO­BATS)

SAGID ALI DESTA PLATE SPIN­NING COM­E­DY ACT.(AFRICAN CIR­CUS AC­RO­BATS)

for book­ings con­tact win­ston rud­dle www.​african-cir­cus .​tz.​com

for book­ings con­tact win­ston rud­dle www.​african-cir­cus .​tz.​com

The Dis­ci­ples - African Hori­zons - DUB PLATE 3 - 1987

The Dis­ci­ples - African Hori­zons - DUB PLATE 3 - 1987

The Dis­ci­ples - African hori­zons MiX 1+ MiX 2 DUB * Dis­ci­ples Vin­tage - KiLLER DUB * Dub Plate 3 - Lis­ten

The Dis­ci­ples - African hori­zons MiX 1+ MiX 2 DUB * Dis­ci­ples Vin­tage - KiLLER DUB * Dub Plate 3 - Lis­ten

((Area of vol­canic ge­ol­o­gy in Saudi Ara­bia.))

((Area of vol­canic ge­ol­o­gy in Saudi Ara­bia.))

Vol­can­ism is dis­tribut­ed asym­met­ri­cal­ly with re­spect to the Red Sea. Large areas are cov­ered with basalt on the Saudi Ara­bi­an Plate. No vol­can­ism has oc­curred at sim­i­lar lat­i­tudes on the African Plate. A large (70000 square miles; 180000 square km) al­ka­li basalt province is lo­cat­ed on the Ara­bi­an Plate in Saudi Ara­bia. This vol­can­ism is re­lat­ed to the rift­ing of the Ara­bi­an and African plates and the for­ma­tion of the Red Sea. Prior to rift­ing, the area was a sta­ble cra­ton. Vol­can­ism began about 40-50 mil­lion years ago as the crust was stretched lat­er­al­ly. Most of the rift­ing and vol­can­ism has oc­curred in the last 30 mil­lion years. In the last 5 mil­lion years, vol­can­ism along the di­ver­gent plate bound­ary be­neath the Red Sea has pro­duced tholeitic basalt, sim­i­lar to basalts at mid-ocean ridge..

Vol­can­ism is dis­tribut­ed asym­met­ri­cal­ly with re­spect to the Red Sea. Large areas are cov­ered with basalt on the Saudi Ara­bi­an Plate. No vol­can­ism has oc­curred at sim­i­lar lat­i­tudes on the African Plate. A large (70000 square miles; 180000 square km) al­ka­li basalt province is lo­cat­ed on the Ara­bi­an Plate in Saudi Ara­bia. This vol­can­ism is re­lat­ed to the rift­ing of the Ara­bi­an and African plates and the for­ma­tion of the Red Sea. Prior to rift­ing, the area was a sta­ble cra­ton. Vol­can­ism began about 40-50 mil­lion years ago as the crust was stretched lat­er­al­ly. Most of the rift­ing and vol­can­ism has oc­curred in the last 30 mil­lion years. In the last 5 mil­lion years, vol­can­ism along the di­ver­gent plate bound­ary be­neath the Red Sea has pro­duced tholeitic basalt, sim­i­lar to basalts at mid-ocean ridge..

BRAHIM SPE­CI­AAAAAAAAAAAAAL DUB PLATE "VOTE"!!!!!!!! POUR AFRICAN HER­ITAGE SOUND

BRAHIM SPE­CI­AAAAAAAAAAAAAL DUB PLATE "VOTE"!!!!!!!! POUR AFRICAN HER­ITAGE SOUND

AFRICAN LIP PLATE WOMEN

AFRICAN LIP PLATE WOMEN

www.​intmensorg.​info

www.​intmensorg.​info

Rift Val­ley - Iten, Kenya (Jan­uary 2010)

Rift Val­ley - Iten, Kenya (Jan­uary 2010)

The Great Rift Val­ley is a name given in the late 19th cen­tu­ry by British ex­plor­er John Wal­ter Gre­go­ry to the con­tin­u­ous ge­o­graph­ic trench, ap­prox­i­mate­ly 6000 kilo­me­tres (3700 mi) in length, that runs from north­ern Syria in South­west Asia to cen­tral Mozam­bique in East Africa. The name con­tin­ues in some us­ages, al­though it is today con­sid­ered ge­o­log­i­cal­ly im­pre­cise as it com­bines fea­tures that are today re­gard­ed as sep­a­rate, al­though re­lat­ed, rift and fault sys­tems. Today, the term is most often used to refer to the val­ley of the East African Rift, the di­ver­gent plate bound­ary which ex­tends from the Afar Triple Junc­tion south­ward across east­ern Africa, and is in the pro­cess of split­ting the African Plate into two new sep­a­rate plates. Ge­ol­o­gists gen­er­al­ly refer to these in­cip­i­ent plates as the Nu­bian Plate and the So­ma­li Plate.

The Great Rift Val­ley is a name given in the late 19th cen­tu­ry by British ex­plor­er John Wal­ter Gre­go­ry to the con­tin­u­ous ge­o­graph­ic trench, ap­prox­i­mate­ly 6000 kilo­me­tres (3700 mi) in length, that runs from north­ern Syria in South­west Asia to cen­tral Mozam­bique in East Africa. The name con­tin­ues in some us­ages, al­though it is today con­sid­ered ge­o­log­i­cal­ly im­pre­cise as it com­bines fea­tures that are today re­gard­ed as sep­a­rate, al­though re­lat­ed, rift and fault sys­tems. Today, the term is most often used to refer to the val­ley of the East African Rift, the di­ver­gent plate bound­ary which ex­tends from the Afar Triple Junc­tion south­ward across east­ern Africa, and is in the pro­cess of split­ting the African Plate into two new sep­a­rate plates. Ge­ol­o­gists gen­er­al­ly refer to these in­cip­i­ent plates as the Nu­bian Plate and the So­ma­li Plate.

Vul­cano

Vul­cano

(video 2005, Ae­o­lian is­lands, Italy). Vul­cano is a small vol­canic is­land in the Tyrrhe­ni­an Sea , about 25 km north of Sici­ly and the south­ern­most of the eight Ae­o­lian Is­lands. It is 21 square kilo­me­ters in area, rises to 499 me­ters, and con­tains sev­er­al vol­canic cen­ters, in­clud­ing one of four ac­tive non-sub­ma­rine vol­ca­noes in Italy. The vol­canic ac­tiv­i­ty in the re­gion is large­ly the re­sult of the north­ward-mov­ing African Plate meet­ing the Eurasian Plate. There are three vol­canic cen­tres on the is­land: At the south­ern end of the is­land are old stra­to­vol­cano cones, Monte Aria (500 m), Monte Sara­ceno (481 m) and Monte Luc­cia (188 m), which have par­tial­ly col­lapsed into the Il Piano Caldera. The most re­cent­ly ac­tive cen­tre is the Gran Cratere at the top of the Fossa cone, the cone hav­ing grown in the Lentia Caldera in the mid­dle of the is­land, and has had at least 7 major erup­tions in the last 6000 years. At the north of the is­land is Vul­canel­lo, 123 me­tres high, and is con­nect­ed to the rest of it by an isth­mus which is flood­ed in bad weath­er. It emerged from the sea dur­ing an erup­tion in 183 BC as a sep­a­rate islet. Oc­ca­sion­al erup­tions from its three cones with both py­ro­clas­tic flow de­posits and lavas oc­curred from then until 1550, the last erup­tion cre­at­ing a nar­row isth­mus con­nect­ing it to Vul­cano. Vul­cano has been quiet since the erup­tion of the Fossa cone on Au­gust 3, 1888 to 1890, which de­posit­ed about 5 me­tres of py­ro­clas­tic ma­te­ri­al on the sum­mit. The style of <b>...</b>

(video 2005, Ae­o­lian is­lands, Italy). Vul­cano is a small vol­canic is­land in the Tyrrhe­ni­an Sea , about 25 km north of Sici­ly and the south­ern­most of the eight Ae­o­lian Is­lands. It is 21 square kilo­me­ters in area, rises to 499 me­ters, and con­tains sev­er­al vol­canic cen­ters, in­clud­ing one of four ac­tive non-sub­ma­rine vol­ca­noes in Italy. The vol­canic ac­tiv­i­ty in the re­gion is large­ly the re­sult of the north­ward-mov­ing African Plate meet­ing the Eurasian Plate. There are three vol­canic cen­tres on the is­land: At the south­ern end of the is­land are old stra­to­vol­cano cones, Monte Aria (500 m), Monte Sara­ceno (481 m) and Monte Luc­cia (188 m), which have par­tial­ly col­lapsed into the Il Piano Caldera. The most re­cent­ly ac­tive cen­tre is the Gran Cratere at the top of the Fossa cone, the cone hav­ing grown in the Lentia Caldera in the mid­dle of the is­land, and has had at least 7 major erup­tions in the last 6000 years. At the north of the is­land is Vul­canel­lo, 123 me­tres high, and is con­nect­ed to the rest of it by an isth­mus which is flood­ed in bad weath­er. It emerged from the sea dur­ing an erup­tion in 183 BC as a sep­a­rate islet. Oc­ca­sion­al erup­tions from its three cones with both py­ro­clas­tic flow de­posits and lavas oc­curred from then until 1550, the last erup­tion cre­at­ing a nar­row isth­mus con­nect­ing it to Vul­cano. Vul­cano has been quiet since the erup­tion of the Fossa cone on Au­gust 3, 1888 to 1890, which de­posit­ed about 5 me­tres of py­ro­clas­tic ma­te­ri­al on the sum­mit. The style of <b>...</b>

lip plate woman drink­ing

lip plate woman drink­ing

the older the women ,the larg­er the ce­ram­ic plate.

the older the women ,the larg­er the ce­ram­ic plate.

Na­tion­al An­them of Madeira Au­tonomous Re­gion

Na­tion­al An­them of Madeira Au­tonomous Re­gion

Na­tion­al An­them of Madeira Au­tonomous Re­gion It is one of the Au­tonomous re­gions of Por­tu­gal, with Madeira Is­land and Porto Santo Is­land being the only in­hab­it­ed is­lands. Al­though it is part of the African Plate, some 650 km (400 mi) off coast Africa, it be­longs po­lit­i­cal­ly and cul­tur­al­ly to Eu­rope, some 860 km (535 mi) from the main­land. For More In­for­ma­tion please visit www.​nationalanthems.​us

Na­tion­al An­them of Madeira Au­tonomous Re­gion It is one of the Au­tonomous re­gions of Por­tu­gal, with Madeira Is­land and Porto Santo Is­land being the only in­hab­it­ed is­lands. Al­though it is part of the African Plate, some 650 km (400 mi) off coast Africa, it be­longs po­lit­i­cal­ly and cul­tur­al­ly to Eu­rope, some 860 km (535 mi) from the main­land. For More In­for­ma­tion please visit www.​nationalanthems.​us

The Vol­cano Song Tik-Tok Par­o­dy

The Vol­cano Song Tik-Tok Par­o­dy

Year 8 Ge­og­ra­phy home­work Lyrics- Wake up in the morn­ing; vol­cano's what I see, I bet­ter get away be­fore it de­stroys my city, One plate is mov­ing down and the pres­sure builds up, I bet­ter get away be­fore it erupts. Smoke is in the air, air I am re­al­ly scared, scared Peo­ple scream­ing ev­ery­where, where VOL­CANO! Those tec­ton­ic plates, plates Re­al­ly aren't my mates, mates We need to evac­u­ate I'm scared re­al­ly scared There is thick smoke ev­ery­where Con­vec­tion cur­rents move the crust now the bound­ary's going bust Con­ver­gent plates are re­al­ly not my mates no, Oh-woah-wa-oh Oh-woah-wa-oh Then bang it erupts Red-hot magma's com­ing up From the man­tle, it burnt the crust. Now the vol­cano blow­ing up I'm scared re­al­ly scared. I bet­ter get away be­fore I am dead oh I am dead The crust of the earth is in lit­tle parts With the man­tle un­der­neath and iron core at the heart De­cay­ing ra­dioac­tive waste heats the man­tle up It burns sub­sid­ing crust and then vol­ca­noes spring up. Lava rocks rain­ing down, down Peo­ple scream­ing re­al­ly loud, loud Smell of burn­ing all around, round VOL­CANO! I can­not see clear­ly I'm felling kinda weary Why do I live in Chile? II live in Chile I'm scared re­al­ly scared There is thick smoke ev­ery­where Con­vec­tion cur­rents move the crust now the bound­ary's going bust Con­ver­gent plates are re­al­ly not my mates no, Oh-woah-wa-oh Oh-woah-wa-oh Then bang it erupts Red-hot magma's com­ing up From the man­tle, it burnt the crust. Now the vol­cano blow­ing up I'm scared re­al­ly scared <b>...</b>

Year 8 Ge­og­ra­phy home­work Lyrics- Wake up in the morn­ing; vol­cano's what I see, I bet­ter get away be­fore it de­stroys my city, One plate is mov­ing down and the pres­sure builds up, I bet­ter get away be­fore it erupts. Smoke is in the air, air I am re­al­ly scared, scared Peo­ple scream­ing ev­ery­where, where VOL­CANO! Those tec­ton­ic plates, plates Re­al­ly aren't my mates, mates We need to evac­u­ate I'm scared re­al­ly scared There is thick smoke ev­ery­where Con­vec­tion cur­rents move the crust now the bound­ary's going bust Con­ver­gent plates are re­al­ly not my mates no, Oh-woah-wa-oh Oh-woah-wa-oh Then bang it erupts Red-hot magma's com­ing up From the man­tle, it burnt the crust. Now the vol­cano blow­ing up I'm scared re­al­ly scared. I bet­ter get away be­fore I am dead oh I am dead The crust of the earth is in lit­tle parts With the man­tle un­der­neath and iron core at the heart De­cay­ing ra­dioac­tive waste heats the man­tle up It burns sub­sid­ing crust and then vol­ca­noes spring up. Lava rocks rain­ing down, down Peo­ple scream­ing re­al­ly loud, loud Smell of burn­ing all around, round VOL­CANO! I can­not see clear­ly I'm felling kinda weary Why do I live in Chile? II live in Chile I'm scared re­al­ly scared There is thick smoke ev­ery­where Con­vec­tion cur­rents move the crust now the bound­ary's going bust Con­ver­gent plates are re­al­ly not my mates no, Oh-woah-wa-oh Oh-woah-wa-oh Then bang it erupts Red-hot magma's com­ing up From the man­tle, it burnt the crust. Now the vol­cano blow­ing up I'm scared re­al­ly scared <b>...</b>

Sci­en­tif­ic Mir­a­cles Of The Holy Quran 15 (Three Stages of Fetal de­vel­op­ment) & the Dead sea

Sci­en­tif­ic Mir­a­cles Of The Holy Quran 15 (Three Stages of Fetal de­vel­op­ment) & the Dead sea

Islam Is The Only Truth The Dead Sea (He­brew: יָם הַ‏‏מֶּ‏‏לַ‏ח‎, "Sea of Salt"; Ara­bic: البَحْر المَيّت‎, "Dead Sea";) is a salt lake be­tween Is­rael and the West Bank to the west, and Jor­dan to the east. It is 422 me­tres (1385 ft) below sea level,[2] and its shores are the low­est point on the sur­face of Earth on dry land. The Dead Sea is 378 m (1240 ft) deep, the deep­est hy­per­saline lake in the world. It is also one of the world's salti­est bod­ies of water, with 33.7% salin­i­ty. Only Lake Assal (Dji­bouti), Garabogazköl and some hy­per­saline lakes of the Mc­Mur­do Dry Val­leys in Antarc­ti­ca (such as Don Juan Pond and per­haps Lake Vanda) have a high­er salin­i­ty. It is 8.6 times as salty as the ocean.[3] This salin­i­ty makes for a harsh en­vi­ron­ment where an­i­mals can­not flour­ish, hence its name. The Dead Sea is 67 kilo­me­tres (42 mi) long and 18 kilo­me­tres (11 mi) wide at its widest point. It lies in the Jor­dan Rift Val­ley, and its main trib­u­tary is the Jor­dan River.​The Dead Sea has at­tract­ed vis­i­tors from around the Mediter­ranean basin for thou­sands of years. Bib­li­cal­ly, it was a place of refuge for King David. It was one of the world's first health re­sorts (for Herod the Great), and it has been the sup­pli­er of a wide va­ri­ety of prod­ucts, from balms for Egyp­tian mum­mi­fi­ca­tion to potash for fer­til­iz­ers. Peo­ple also use the salt and the min­er­als from the Dead Sea to cre­ate cos­met­ics and herbal sa­chets. The Dead Sea is an en­dorhe­ic lake lo­cat­ed in the Jor­dan Rift Val­ley, a <b>...</b>

Islam Is The Only Truth The Dead Sea (He­brew: יָם הַ‏‏מֶּ‏‏לַ‏ח‎, "Sea of Salt"; Ara­bic: البَحْر المَيّت‎, "Dead Sea";) is a salt lake be­tween Is­rael and the West Bank to the west, and Jor­dan to the east. It is 422 me­tres (1385 ft) below sea level,[2] and its shores are the low­est point on the sur­face of Earth on dry land. The Dead Sea is 378 m (1240 ft) deep, the deep­est hy­per­saline lake in the world. It is also one of the world's salti­est bod­ies of water, with 33.7% salin­i­ty. Only Lake Assal (Dji­bouti), Garabogazköl and some hy­per­saline lakes of the Mc­Mur­do Dry Val­leys in Antarc­ti­ca (such as Don Juan Pond and per­haps Lake Vanda) have a high­er salin­i­ty. It is 8.6 times as salty as the ocean.[3] This salin­i­ty makes for a harsh en­vi­ron­ment where an­i­mals can­not flour­ish, hence its name. The Dead Sea is 67 kilo­me­tres (42 mi) long and 18 kilo­me­tres (11 mi) wide at its widest point. It lies in the Jor­dan Rift Val­ley, and its main trib­u­tary is the Jor­dan River.​The Dead Sea has at­tract­ed vis­i­tors from around the Mediter­ranean basin for thou­sands of years. Bib­li­cal­ly, it was a place of refuge for King David. It was one of the world's first health re­sorts (for Herod the Great), and it has been the sup­pli­er of a wide va­ri­ety of prod­ucts, from balms for Egyp­tian mum­mi­fi­ca­tion to potash for fer­til­iz­ers. Peo­ple also use the salt and the min­er­als from the Dead Sea to cre­ate cos­met­ics and herbal sa­chets. The Dead Sea is an en­dorhe­ic lake lo­cat­ed in the Jor­dan Rift Val­ley, a <b>...</b>

Child Nu­tri­tion: A Healthy Plate for Cul­tur­al Foods

Child Nu­tri­tion: A Healthy Plate for Cul­tur­al Foods

The Cen­tral Val­ley has a di­verse pop­u­la­tion, and that means our chil­dren can enjoy many dif­fer­ent cul­tur­al foods. But what is the best way to en­sure a healthy plate for African-Amer­i­can and Lati­no dish­es? Reg­is­tered Di­eti­tian Dr. Con­nie Schnei­der and her col­leagues will show us how. 0 to 5 in 30 Min­utes! is a prod­uct of Val­ley Pub­lic Tele­vi­sion. The pro­gram is spon­sored by First 5 Fres­no Coun­ty and First 5 Tu­lare Coun­ty.

The Cen­tral Val­ley has a di­verse pop­u­la­tion, and that means our chil­dren can enjoy many dif­fer­ent cul­tur­al foods. But what is the best way to en­sure a healthy plate for African-Amer­i­can and Lati­no dish­es? Reg­is­tered Di­eti­tian Dr. Con­nie Schnei­der and her col­leagues will show us how. 0 to 5 in 30 Min­utes! is a prod­uct of Val­ley Pub­lic Tele­vi­sion. The pro­gram is spon­sored by First 5 Fres­no Coun­ty and First 5 Tu­lare Coun­ty.

Core-man­tle bound­ary to­pog­ra­phy pre­sen­ta­tion

Core-man­tle bound­ary to­pog­ra­phy pre­sen­ta­tion

Avalanch­ing and its in­flu­ence on the to­pog­ra­phy of the core-man­tle bound­ary.

Avalanch­ing and its in­flu­ence on the to­pog­ra­phy of the core-man­tle bound­ary.

Congo Ashan­ti Roy Singers And Play­ers African Blood OnU­Sound

Congo Ashan­ti Roy Singers And Play­ers African Blood OnU­Sound

Congo Ashan­ti Roy (From Singers And Play­ers) - African Blood - Taken From The "Disco Plate Col­lec­tion Vol 1" Album - On U Sound Records - Down­load en­tire CD @ www.​myspace.​com or @ www.​4shared.​com

Congo Ashan­ti Roy (From Singers And Play­ers) - African Blood - Taken From The "Disco Plate Col­lec­tion Vol 1" Album - On U Sound Records - Down­load en­tire CD @ www.​myspace.​com or @ www.​4shared.​com

2010 L'OR­MARINS QUEEN'S PLATE (GR1)

2010 L'OR­MARINS QUEEN'S PLATE (GR1)

POCK­ET POWER (Jet Mas­ter x Stormsvlei) 9 Jan­uary 2010 R1mil­lion L'Or­marins Queen's Plate Turf 1600m Ke­nil­worth Race­course, South Africa Owner : Marsh Shirtliff, Arthur and Rina Web­ber Train­er : Mike Bass Jock­ey : Bernard Fayd'Herbe Breed­er : Zand­vli­et Stud "The Peo­ple's Cham­pi­on" Re­sult : 1st Pock­et Power 2nd Kapil 3rd Big City Life 3th Fabi­ani

POCK­ET POWER (Jet Mas­ter x Stormsvlei) 9 Jan­uary 2010 R1mil­lion L'Or­marins Queen's Plate Turf 1600m Ke­nil­worth Race­course, South Africa Owner : Marsh Shirtliff, Arthur and Rina Web­ber Train­er : Mike Bass Jock­ey : Bernard Fayd'Herbe Breed­er : Zand­vli­et Stud "The Peo­ple's Cham­pi­on" Re­sult : 1st Pock­et Power 2nd Kapil 3rd Big City Life 3th Fabi­ani

Plate Tec­ton­ics - Les­son 4 - Part 2 of 8

Plate Tec­ton­ics - Les­son 4 - Part 2 of 8

Plan­et of Man Se­ries -- Jig­saw Fit (30min­utes) Host; Tuzo Wil­son Plate Tec­ton­ics - Les­son 4 - Part 2 of 8 •Early 70's plate tec­ton­ics -- enig­ma of moun­tains dis­cov­ered with the the­o­ry of plate tec­ton­ics •An­i­ma­tion il­lus­trat­ing the slabs of in­di­vid­u­al plates from around the world. •Crust 60 miles thick •Iso­stat­ic re­bound from the last ice age. • Hud­son Bay is dis­tin­gu­sished from this pro­cess by a in­dis­ntct shore­line and raised beach's •Plate name -- Eu­arasian In­do-Aus­tralian, African, Amer­i­can , Antarc­tic, Nazca, Pa­cif­ic Plates. • Rock Types - Basalt at the tops of the spread­ing bound­aries, upper layer of the plate, Pe­ri­odi­tite (mag­ne­sium rich) lower layer of the plate. •Un­der­wa­ter erup­tion -- lava come into con­tact with the cold water forms pil­low like shapes "Pil­low lava" •Footage show­ing un­der­wa­ter erup­tions. •Ice­land -- en­tire­ly cre­at­ed from the spread­ing ridge of an ac­tive zone. •Ice­land Geother­mal uses • Mid-At­lantic ocean­ic ridge fol­lows the shore­lines of both Africa and South Amer­i­ca. 200 mil­lion years to open to its cur­rent width. •Red Sea clear­ly shows also how Africa and Ara­bia fit­ted to­geth­er/. •East Africa -- Great Rift Val­ley, early sep­a­ra­tion of this pro­cess like the Red Sea sep­a­ra­tion. The en­tire Rift Val­ley has vol­can­ism. •Trans­form fault -- no moun­tains and no vol­ca­noes but earth­quakes are pro­duced. It's the re­sult of plates slid­ing past one an­oth­er. These in­tense earth­quakes occur most­ly in the deep ocean basins. But some­times they come on the con­ti­nent <b>...</b>

Plan­et of Man Se­ries -- Jig­saw Fit (30min­utes) Host; Tuzo Wil­son Plate Tec­ton­ics - Les­son 4 - Part 2 of 8 •Early 70's plate tec­ton­ics -- enig­ma of moun­tains dis­cov­ered with the the­o­ry of plate tec­ton­ics •An­i­ma­tion il­lus­trat­ing the slabs of in­di­vid­u­al plates from around the world. •Crust 60 miles thick •Iso­stat­ic re­bound from the last ice age. • Hud­son Bay is dis­tin­gu­sished from this pro­cess by a in­dis­ntct shore­line and raised beach's •Plate name -- Eu­arasian In­do-Aus­tralian, African, Amer­i­can , Antarc­tic, Nazca, Pa­cif­ic Plates. • Rock Types - Basalt at the tops of the spread­ing bound­aries, upper layer of the plate, Pe­ri­odi­tite (mag­ne­sium rich) lower layer of the plate. •Un­der­wa­ter erup­tion -- lava come into con­tact with the cold water forms pil­low like shapes "Pil­low lava" •Footage show­ing un­der­wa­ter erup­tions. •Ice­land -- en­tire­ly cre­at­ed from the spread­ing ridge of an ac­tive zone. •Ice­land Geother­mal uses • Mid-At­lantic ocean­ic ridge fol­lows the shore­lines of both Africa and South Amer­i­ca. 200 mil­lion years to open to its cur­rent width. •Red Sea clear­ly shows also how Africa and Ara­bia fit­ted to­geth­er/. •East Africa -- Great Rift Val­ley, early sep­a­ra­tion of this pro­cess like the Red Sea sep­a­ra­tion. The en­tire Rift Val­ley has vol­can­ism. •Trans­form fault -- no moun­tains and no vol­ca­noes but earth­quakes are pro­duced. It's the re­sult of plates slid­ing past one an­oth­er. These in­tense earth­quakes occur most­ly in the deep ocean basins. But some­times they come on the con­ti­nent <b>...</b>

African Dance Nor­wich Lord Mayor's Day 2010

African Dance Nor­wich Lord Mayor's Day 2010

A snip­pet of this clever act I en­joyed out­side The Forum in Nor­wich. I saw them ar­rive in a taxi, but not sure where from.

A snip­pet of this clever act I en­joyed out­side The Forum in Nor­wich. I saw them ar­rive in a taxi, but not sure where from.