| 
  The Rock 
  Strong
  | 
Gibraltar - History and Geography
 
When you first see the Rock of Gibraltar, whether it is from  the 
air, from the sea or from either the Costa del Sol or the western 
end  of the Bay, it is its impressive stature, towering  isolated 
above  the  surrounding  countryside, that  causes  the  greatest 
impact.  It has had this effect on  people for many thousands  of 
years. 
 
Gibraltar is a beacon which signals the position of the Strait of 
Gibraltar, the narrow neck which separates Europe from Africa and 
provides  the  only  link  between the  Atlantic  Ocean  and  the 
Mediterranean Sea.  
 
On the 3rd of March 1848 a skull was found in Forbes's Quarry  at 
the foot of the sheer north face of the Rock of Gibraltar. 
 
Nobody knew it at the time but it belonged not to a modern human, 
like  us, but to a prehistoric form. It was put away and  another 
found eight years later in the Neander Valley near Dusseldorf  in 
Germany  gave this human its name - instead of Gibraltar  Man  it 
became Neanderthal Man - Gibraltar missed out.
 
This is not the only Neanderthal from Gibraltar. Another, a young 
child's broken skull, was found nearby in 1928, in a rock shelter 
known as Devil's Tower. Talk today to experts from the  Gibraltar 
Museum or from the Natural History Museum in London and they will 
tell  you that other caves in Gibraltar were also home  to  these 
people as far back as 120 thousand years ago or more. Excavations 
even today continue to produce exciting finds.
 
Many  sites used by Neanderthals were situated  where  impressive 
features  of the landscape made them easy to find.  If you  drive 
along  the  coast road eastwards from Malaga on a clear  day  you 
will  see in the distance on your left a  horseshoe-shaped  pass, 
protected  on either side by cliffs. The shape is  quite  unusual 
and  very much a landmark. On those distant cliffs lies the  cave 
of  Zafarraya, another Neanderthal site. If you travel west  from 
Malaga,  the  landform  which strikes you most  is  the  Rock  of 
Gibraltar so it is not surprising that it was so important to the 
Neanderthals.
 
The  Neanderthals once roamed over much of Europe and the  Middle 
East.  Then, as modern humans emerged from the African  continent 
and  began  to spread across Europe and  Asia,  the  Neanderthals 
somehow  lost  out.  As the waves of modern  humans  spread,  the 
Neanderthals  became extinct, first in the Middle East,  then  in 
eastern  Europe, then western Europe and finally south  into  the 
Iberian  Peninsula. It seems probable now that Gibraltar was  one 
of the last places where these Neanderthals survived, clinging on 
to  their  way of life in the face of overwhelming  odds  against 
them.
 
This  beacon  which  attracted the  early  inhabitants  had  many 
advantages  as  a  home.  Being  limestone,  the  Rock  which  is 
geologically  very different from the surrounding  landscape,  is 
riddled  with caves. Over 140 have been discovered so far.  Those 
which had openings to the outside world made perfect shelters.  
The  climate was also colder than today which meant that the  sea 
level  was  lower: off the eastern cliffs of the  Rock  a  large, 
flat,   sandy   plain   stretched   out   towards   the   distant 
Mediterranean.  It  was  full of good hunting.  There  were  many 
rabbits,  red deer, wild cattle and horse along with now  extinct 
species  of  elephant and rhinoceros; on the  cliffs  there  were 
ibexes, wild mountain goats.  
 
The  scene  was close to paradise for the  early  inhabitants  of 
Gibraltar.  The  hunting  was so good  that  it  attracted  other 
predators, especially hyenas, leopards and lions. So these people 
must have forayed with caution.
 
So  why is Gibraltar, a lump of limestone, so different from  the 
surrounding countryside? It all has to do with events which  took 
place  long before any kind of human had appeared on the face  of 
the earth. The first thing to remember is that limestone is  made 
up  of  millions  of small shelled animals which  have  died  and 
settled  in  the sea bed; slowly these shells harden  and  become 
rock. 
 
So  another point to remember is that when you walk on  the  Rock 
you are stepping on an ancient sea bed Imagine then, for millions 
of  years, a mass of limestone is growing under the sea. This  is 
happening  around  200  million years ago.  The  continents  look 
nothing like they do today. Dinosaurs roam the land. Slowly  over 
millions  of years the continents assume their present shape.  As 
Africa  barges  into Europe, the land folds  and  forms  mountain 
chains  like  the  Alps. Other chunks are  pushed  out  of  their 
position.  One piece is thrust westwards and comes to rest  where 
Gibraltar  is today.  It is very different from  the  surrounding 
countryside which is made up of younger rocks.
 
The story does not end there. The pressures continue and flip the 
Rock  over on its back. The spine of the Rock, from the radar  on 
the  north  side,  to  the top Cable  Car  Station,  to  O'Hara's 
Battery,  was once its base! As all this is happening   and   for  
many   years afterwards, the Rock sinks and is  uplifted  several 
times; the sea rises and falls. The Rock is an island, then is  a 
part  of the mainland with a wider coastline than today,  and  so 
on.  The climate  changes:  tropical,  cold, Mediterranean  -  it 
keeps changing as do the animals and plants which live on it.  
Winds  blow with force and push sands against its  eastern  side, 
forming  a  huge sand dune: it is still there today,  covered  in 
parts  by  the corrugated sheets of  the  watercatchments.  These 
winds  shape  the Rock. Waves lash against cliffs which  are  now 
suspended  more than half way up the Rock. They too  carve  their 
signature.  Shaping  takes  place  inside  as  well  as  outside: 
rainwater  percolates  through  the  Rock  along  the  lines   of 
weakness,  creating cracks, fissures, and eventually  caves.  All 
these processes are still at work today, eroding and changing the 
shape  of Gibraltar, so slowly that we cannot see it  within  our 
short life spans. Eventually, millions of years from now, it will 
have lost all semblance of its present shape.
 
For now it remains as a narrow peninsula stuck to the end of  the 
Iberian  Peninsula,  linked  to  it by  a  narrow  isthmus.  This 
isthmus,  covered  by buildings and a runway, is sandy.  You  can 
still  see this sand on the surface in places, often littered  in 
marine  shells  from a more recent past when  the  sea  separated 
Gibraltar from the rest. This would have last happened during the 
latest  warm  period  of the  glaciations,  probably  around  120 
thousand  years ago. Many still refer to Gibraltar as an  island. 
Historically,  biologically,  even  politically it  has  been  an 
island even in recent times, but physically it is a peninsula.
 
The   peninsula   of  Gibraltar  is geographically  divided  into 
several  zones. The eastern side of its six kilometre length,  is 
made  up  of  sheer cliffs, reaching a maximum  altitude  of  426 
metres above sea level close to O'Hara's  Battery.  The  base  is 
dominated by the massive prehistoric sand dune and by tall slopes 
on either side. These slopes are largely the product of years  of 
rock falls as pieces of the Rock continue to collapse towards the 
sea  when rain dislodges the loose boulders. Sandy  beaches  form 
the perimeter where this mass of rock and sand meets the sea. The 
western  half  is  very different. Its  slopes  are  gentler  and 
gradually  reach the sea. Much of its lower half is taken  up  by 
the city and the urban zone has spread westwards, within the port 
area, in recent years as land has been reclaimed from the sea.
 
The  upper  parts are a nature reserve.  This  western  side  has 
never  had the large expanses of prehistoric sand of the  eastern 
side  -  the gradient steepens offshore and the Bay is  over  800 
metres deep, as deep as the North Sea!
 
To  the  south  of  the main mass of  the  Rock  there  are  rock 
platforms,  a higher plateau known as Windmill Hill, a lower  one 
known  as  Europa Flats, and narrower and lower segments  on  the 
fringes,  forming  rocky  beaches. These  plateaux  are  wave-cut 
platforms - they mark former sea levels and are clearly visible.
 
When the ancient mariners from the east arrived in this region in 
the  eighth  century BC, they once again homed in on  the  beacon 
which  was  the Rock and were attracted to large  marine  caverns 
close  to these southern platforms. We know that Phoenicians  and 
ancient Greeks came here. It has also been suggested by some,  on 
the  basis  of  cave paintings of sailing  ships  in  caves  near 
Gibraltar,   that   perhaps  even  earlier   civilisations,   the 
Mycaeneans  for example, might have sailed to the Strait  as  far 
back as the sixteenth century BC.
 
Whichever  way,  the  Strait  and the  Rock  were  known  in  the 
classical  eastern  Mediterranean  world.  According  to   legend 
Hercules  passed through here to take the cattle of Geryon -  his 
tenth  labour  - and opened up the Strait, creating  the  pillars 
which  received his name (Hercules to the Romans). These  pillars 
are  still clearly identifiable today: the Rock of  Gibraltar  on 
one  side and the Jbel Musa on the other. The legend matches  the 
scientific   reality   although  the  timescales   are   somewhat 
different.  
 
The last time the Strait opened up was around five million  years 
ago and there were no humans around to watch it happen.  It  must  
have  been  a spectacular  event  indeed.  The Mediterranean  had 
been  land-locked for a very long time and had evaporated.   Then 
as  a fissure developed where the Strait is today,  the  Atlantic 
gushed  in  filling the basin in just one hundred years,  with  a 
huge ten thousand foot waterfall at the entrance to the Strait.
 
Respect  for the sea and fear of the unknown must have  dominated 
the  lives of the ancients as many perished in their small  ships 
during  violent storms as is clear from reading an  ancient  text 
such  as  Homer's Odyssey. The Strait is a narrow  channel  which 
funnels  winds.   Violent  storms  develop  quickly  with  little 
notice, especially from the east and south-west. These winds have 
been known to sailors from time immemorial - the east winds,  for 
example, are known as Levantes. 
 
The  idea  of  venturing past the channel must  have  filled  the 
ancients  with trepidation - it was only their curiosity and  the 
lure  of mineral and other resources beyond which made them  take 
the risk.
 
They  took the risks with certain safeguards. One of the  caverns 
at the foot of the northern pillar, known today as Gorham's Cave, 
was  a  place of worship, a shrine. Many  pieces  of  Phoenician, 
Carthaginian  and Greek pottery have been found here  along  with 
glass  beads, amulets and scarabs bearing classical and  Egyptian 
gods.   Many  of  the ancient references to  caves  on  the  Rock 
probably related to Gorham's Cave.
 
For many years Gibraltar continued in its role as stopping  point 
and place of worship but nobody seems to have settled on it.  The 
Phoenicians preferred sites on river estuaries or upstream - they 
had settlements by rivers close to the Rock. The Romans, too  had 
cities  nearby but never built one on Gibraltar.  It was  with  a 
new  cultural wave, much later on, that the basis for a city  was 
established....
 
It  happened in the month of April in the year 711 AD.  Following 
the  death  of the prophet Mohammed a wave  of  Islamic  conquest 
overran  North Africa from Arabia. By 710 AD it had  reached  the 
shores  of  the  Strait and Europe was  poised  for  the  Islamic 
conquest. 
 
There are various versions of the events but one thing is clear - 
the  Visigoths which had deposed the Romans and ruled Spain  were 
weak  and  divided. The Visigothic Count Julian  who  ruled  over 
Ceuta in North Africa was surrounded and he had a score to settle 
with  his  compatriots on the other side of the  Strait.  So,  to 
divert the Muslims, he offered to assist them in the conquest  of 
Spain.
 
The  assault  was down to a Berber  chief,  Tarik-ibn-Ziyad,  the 
Governor  of Tangier. He sailed across the Strait by night,  from 
Ceuta  not  Tangier  so  as not  to  arouse  suspicion  and  used 
Visigothic  ships. His first attempt on Algeciras failed  but  he 
was successful in landing undetected on Gibraltar from where  the 
conquest  began.  At  that stage the Rock  was  probably  only  a 
bridgehead  and  was only lightly fortified for  the  first  four 
hundred years of occupation.
 
By  the 11th Century AD Gibraltar is part of the Arab kingdom  of 
Seville except for a short period when it comes under Berber rule 
from  Malaga.  The mounting threat of invasion by  North  African 
sects forces the Arab Governor of Algeciras to order in 1068  the 
building  of a fort in Gibraltar. Spain is eventually overrun  by 
another  North  African  sect, the Almohads,  and  it  was  their 
leader,  Al- Mumin, who commanded the building of the first  city 
in Gibraltar - the Medinat al- Fath, the City of Victory. 
 
It  was, by all accounts, an impressive city and its  foundations 
were  laid on the 19th May, 1160. On completion of the works  Al- 
Mumin  personally  crossed the Strait to inspect  the  works  and 
stayed in Gibraltar for two months, inviting all his  subordinate 
kings  to see the works. It is said that AI-Mumin was  especially 
impressed by a large windmill which had been built on the top  of 
the hill.
 
Skirmishing  and fighting continued between 1160 and 1300,  among 
Muslims  or  between  Muslims and Christians. By  1252  only  two 
Islamic  kingdoms were left in Spain, in Murcia and  Granada.  By 
the year 1309, King Ferdinand IV had laid siege on Algeciras and, 
learning of Arab weakness on the Rock sent Alonso Perez de Guzman 
to  capture  it.  Thus Gibraltar endured  its  first  siege.  The 
Spaniards took the Upper Rock from where they bombarded the  town 
using cannon. The garrison surrendered after one month. Gibraltar 
then  had  1500 inhabitants and they were allowed  to  leave  for 
North Africa.
 
The  Spaniards set to repair the fortifications and shipyard  but 
few people wanted to settle in Gibraltar which was considered  to 
be a high risk town. This forced Ferdinand to offer freedom  from 
justice  to  anyone who lived in Gibraltar for one year  and  one 
day.  By  1333 Gibraltar was once more in Muslim hands  as  Abdul 
Malik,  son  of  the king of Morocco, laid  siege.  The  garrison 
surrendered  after four and a half months of siege.  More  sieges 
were  to  follow until 1462 when the Spaniards  finally  captured 
Gibraltar from the Muslims.
 
The strategic value of Gibraltar then declined as it became  just 
another  Spanish provincial town. Few people wanted to settle  on 
the Rock as had happened earlier and the Spanish king, Henry  IV, 
extended  Gibraltar's municipal boundaries to cover much  of  the 
hinterland. The economic and agricultural potential developed but 
at the expense of the defences. 
 
There  were  more sieges  as  Spaniards   besieged  Spaniards  in 
petty  local  feuds.  By 1474 Henry died  and  was  succeeded  by 
Isabella, the Catholic Queen. After the fall of Granada in  1497, 
she  used  Gibraltar as a base port for launching  an  attack  on 
North Africa and in 1499 she used it as a port for the removal of 
exiled Moors from Granada.
 
It  was  Isabella who, tired of the petty  squabbling  among  her 
nobility,  issued  a decree on the 22nd  December,  1501,  making 
Gibraltar crown property. On the 10th July of the following year, 
Gibraltar  received  its Royal Warrant granting it  its  coat  of 
arms.  The  castle and the key, which still survive  today,  were 
given  in recognition of Gibraltar as the key "between these  our 
kingdoms  in  the eastern and western seas and the  sentinel  and 
defence of the Strait of the said seas through which no ships  or 
peoples  of  either of these seas can pass to the  other  without 
sighting or calling at it."
 
By the middle of the sixteenth century a new kind of conflict had 
arisen  as  corsairs  from  the coast  of  Barbary,  under  their 
infamous  leader Barbarossa, hounded the zone. In the  summer  of 
1540  a large fleet of pirates assembled, and raided  the  poorly 
defended Gibraltar. Years later, after mounting pressure from the 
inhabitants  of  Gibraltar,  the Emperor Charles  V  ordered  the 
Italian engineer Calvi to build a protective wall. This wall  was 
extended  to reach the top of the Rock in the reign of Philip  II 
some years later.
 
Life  continued  at  a  slow pace  until  the  beginning  of  the 
eighteenth  century.  Then, on the 17th July, 1704, a council  of 
war  was held aboard the English warship the Royal Catharine  off 
the  North  African town of Tetuan. Four days later  the  English 
fleet, under Admiral Sir George Rooke, entered Gibraltar Bay.  At 
3  pm 1,800 English and Dutch marines were landed on the  isthmus 
with  the Dutch Prince Hesse at the head. Gibraltar was  cut  off 
but the Governor of Gibraltar refused to surrender. 
 
The  days that followed saw a massive bombardment of the town  by 
the  English fleet: on the morning of the 23rd, 1,500  shot  were 
fired  in 5-6 hours against the town. Landings took place in  the 
south and in the morning of the 24th, the Governor capitulated.
 
So  in this way a joint Anglo-Dutch force captured Gibraltar,  on 
behalf  of Charles of Austria who was pretender to the throne  of 
Spain.  Things  took a while to settle down.  Shortly  after  the 
capture a Spanish goatherd, Simon Susarte, led 500 Spanish troops 
to  Europa  Advance  on the south-eastern side of  the  Rock  and 
killed  the  guard. They moved to the Upper Rock  and  spent  the 
night  in St Michael's  Cave. The next morning they attacked  the 
Signal  Station  but  the  alarm  was  raised  and  the   English 
grenadiers counter-attacked. 160 prisoners were taken including a 
colonel and thirty other officers; the rest were killed trying to 
escape.
 
Skirmishes  and  attacks continued for a while. By  1726  trading 
between Gibraltar and Spain had resumed. Then, early in 1727  the 
Spaniards laid siege on  the  Rock but after several unsuccessful 
and costly attempts gave up in June of the same year.
 
The final military siege on Gibraltar followed many years  later, 
in  1779.  On  this occasion the Spaniards  and  French  combined 
forces  and launched a massive onslaught which was to last  close 
to  four years. It was a siege, known as the Great  Siege,  which 
was  to test the ingenuity and will to survive of  the  garrison. 
The first galleries were dug during this time, as Sergeant  Major 
Ince  attempted  to drill a tunnel to place a gun  in  a  vantage 
point  on the Rock. On tunnelling sidewards to  make  ventilation 
shafts  he  realised  that these exits  would  make  perfect  gun 
positions. Later, a Lieutenant Koehler designed a carriage  which 
allowed the guns on the cliffs to be directly pointed down at the 
enemy.   Accounts  of  the siege are full  of  vivid  stories  of 
survival  and daring. On the 21 November, 1781, the defenders  of 
the garrison took the offensive and caught the enemy batteries on 
the  isthmus by surprise, destroying them and setting back  their 
progress: this event is commemorated as the Sortie.
 
Desperate  at  their inability to succeed by land  the  attackers 
changed  to a maritime assault and converted a number of  vessels 
into  floating  batteries, double- hulled, highly  fortified  and 
fire  resistant  ships which were loaded with  guns.   They  were 
placed  opposite the king's Bastion with the object of  making  a 
breach  in the defensive walls. It was hailed as the battle  that 
would finally force Gibraltar to surrender. The enemy had  failed 
to  take one thing into account: the British had been  using  red 
hot  shot,  cannon  balls  fired  after  having  been  heated  in 
furnaces, and these eventually penetrated the strong hulls of the 
floating batteries and caused them to blow up and sink. The siege 
ended soon after.
 
Nineteenth  century  Gibraltar  was at last able  to  develop  in 
relative peace. In the early years it was Nelson's base port  and 
his body was brought here in 1805 after the Battle of  Trafalgar, 
at  the  western end of the Strait of Gibraltar, reputedly  in  a 
barrel  of  rum. It was a period during  which  important  social 
changes  were taking place on the Rock.  Its civilian  community, 
composed  of  British,  Genoese, Portuguese,  Spanish,  Jews  and 
others,  was beginning to establish itself firmly. The  roots  of 
the Gibraltarians of today were being consolidated.
 
The Gibraltarians of today are a friendly people, bilingual, with 
a  unique  sense of religious tolerance. Their  identity  is  now 
firmly consolidated. A number of events contributed towards this. 
The most recent was the closing of the frontier between Spain and 
Gibraltar by General Franco in 1967. This measure had the  effect 
of strengthening the sense of unity of the Gibraltarians so that, 
by  the  time the frontier was re-opened, partially in  1982  and 
fully in  1985,  an unbreakable bond had been formed.  
 
Earlier,  during the second world war, the entire population  was 
evacuated  to  Britain, Madeira and Jamaica. This  mass  movement 
away  from  the  native home had  highlighted  the  features  and 
attributes common to all Gibraltarians and the collective  desire 
to return after the war testified that a people had come of age.
 
The  post war years were characterised by increasing  legislative 
autonomy  culminating in the constitution of 1969  which  created 
the  Gibraltar  House of Assembly,  Gibraltar's  parliament  with 
powers over a wide range of internal affairs.  The  autonomy   of  
the Gibraltarians has strengthened over the years and the mood in 
Gibraltar today is of a people who identify themselves as British 
Gibraltarians and who demand the right to self-determination.
 
Between  Nelson  and  today, Gibraltar  has  therefore  not  only 
changed  socially,  but  it  has  also  changed  physically.  The 
impressive   reclamation  schemes  of  the  last  decade  are   a 
culmination  of  earlier projects. All land below  the  defensive 
walls of Gibraltar is reclaimed from the sea.  
 
In   1894,   the  dockyards, commercial and detached  moles  were 
built, a massive project which was to take 12 years to complete. 
During  the  late nineteenth century and the early years  of  the 
twentieth century Gibraltar's potable water problems, due to  the 
summer droughts characteristic of the climate, were resolved with 
the  excavation of huge reservoirs inside the Rock  which  stored 
rainwater  collected from  catchment areas specially prepared  on 
the  north-western and eastern sides of the Rock. More  recently, 
as  the demands of the population have grown, so  new  technology 
has replaced the old catchments. Today, Gibraltar desalinates sea 
water and is no longer dependent on the unpredictable rainfall.
 
The  strategic  value  of  the Rock  has  continued  during  this 
century.  It  was a port of call for the Mediterranean  and  Home 
fleets.  During the Second World War, the runway was  constructed 
and  was the launchpad for Operation Torch - the allied  landings 
of North Africa. 
 
In  1982,  ships  were refitted for the  Falklands  campaign  and 
Gibraltar  became a stopover for ships and troops.  It  served  a 
similar  function  in  1991 during the Gulf War.  The  Rock,  the 
beacon  which attracted the Gibraltarians of prehistory,  retains 
its powers and charms as it looks towards the 21st Century. 
 
  |