Peninsular Gneiss

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Peninsular Gneiss or Peninsular Gniessic Complex are the

Indian Peninsula, on top of which, the supra-crustal Dharwar System have been laid down.[1] The term was first fashioned by W.F.Smeeth of the Mysore Geological Department in 1916 based on the first scientific study of this rock exposure. One of the best exposures of this rock mass, dated 2.5 to 3.4 billion years, is located at Lal Bagh in Bangalore.[2][3]
The exposure is also called the Lalbagh rock.[4]

Geology

Main article: Geology of India
A light and dark grey area of ground with sporadic ledges and a rough texture. A white rooftop and park concessions are visible in the background.
Exposed gneiss hillock at Lal Bagh
Dharwars of South India

The

Dharwar (Super Group) and the Peninsular Gneissic Complex are the classified groups of the Precambrian rocks of India. The extent of the Archean system is depicted as the dominant system of South India
in the pictured Geological Map of India.

In most stratigraphic schemes, the peninsular gneisses are shown as the younger Archaean strata situated above the

sedimentary–volcogenic sequence are reported as sources of the peninsular gneisses made up of polyphase migmatites, gneisses and granites ranging in composition from granodiorite to tonalite.[5]

The rocks of the Dharwar Group, which are mainly sedimentary in origin, occur in narrow elongated synclines resting on the gneisses found in

Bellary district, Mysore and the Aravallis of Rajputana
.

The

igneous rocks are considered the contributors to formation of the composite gneiss.[3][6]

Geology of the Lalbagh hill monument

Plaque gives history of the Lalbagh and the monument

The Lalbagh hill, which has been declared as a Geological Monument (plaque pictured) to represent the Peninsular Gneiss, has dark

granitic to granodioritic composition containing streaks of biolite. Remnants of older rocks are seen in the form of enclaves.[2] The research information of the geological record of the gneisses, collated and reported in the publication "Geological Monuments of India" published by the Geological Survey of India, is quoted below to provide an undiluted version.[3]

A common enclave is a dark grey to black rock called

lenticular
shapes.

.

The earliest rock was a dark coloured amphibolite which was converted into grey biotite gneiss during migmatization. The grey biotite gneiss during migmatization was first intruded by grey porphyritic granite and later by pink granites. Pegamatities of several generations have traversed all these rocks.

Gneissic exposure at the Lalbagh hillock

Geological age

Initial studies on the Gneiss samples of the Lalbagh hill and other locations in Bengaluru, carried out in the early 1970s, have attributed two major events of 2.9 –3.0

Ga and 2.5 Ga −2.6 Ga for development of the Peninsular Gneisses of Bengaluru. Recent studies carried out with precision techniques indicate that the gneisses have accreted in the following major episodes.[3]

Geological/Radiometric ages Study Region/Belt
3.4 Ga. The oldest Peninsular Gneiss found in areas in the
Holenarsipur – Hunsur
belt
3.3–3.2 Ga. The second generation Peninsular Gneiss found in the Bengaluru–
Chickmagalur
–Holenarsipur region
3.0–2.9 Ga a)
Grandiorite facies in the Bengaluru Gneisses established by the Single Zircon Kober evaporation
207Pb/206 Pb data.

b) In the

Dharwar Craton studies done on the trondhjemites of Holenarsipur, major crust forming event are attributed through the Rb–Sr whole rock isochron
ages.

c) In

Zircons from amphibolite facies gneisses from Kobaladurga and Kober
single zircon evaporation ages of grey gneisses have been considered

Thus, three major episodes, namely, 3.4 Ga., 3.3–3.2 Ga., and 3.0–2.9

Ga., are accreted to form the Peninsular Gneiss of the region, dated 2500 to 3400 million years.[2]

The

suture zones in the Indian subcontinent.[7]

Lalbagh

One of the four Cardinal towers of Bengaluru erected above the Lalbagh hill of Peninsular Gneiss
Further information: Lal Bagh

Vijayanagara empire, who established four cardinal towers setting limits to the growth of the city. One of the towers at the southern end of the city is the Lalbagh tower erected over the Lalbagh hill which is made up of Peninsular Gneiss, now identified as a National Geological Monument. The city has outgrown the limits set by Kempegowda many times and is now part of the downtown area.[9]
The topographic setting of the Lalbagh rock, from a layman's interest, is that in the western and northern directions it slopes steeply while it merges gently with soil in the east and south. View from the North is impressive since the rock has retained its original form. The west or north–west view is panoramic and aesthetic, with grayish–white clean plates like appearance (see picture). The rock shines white after the rains and attracts attention of the visitors who excitedly climb the rock mass to the tower at the top to get a panoramic view of the gardens and the city.[4]

Access

Further information: Bangalore

The monument, located in the southern part of Bengaluru, 4 kilometres (2 mi) from the Legislature office complex of the Karnataka Government (Vidhana Soudha) within the Lalbagh gardens is easily approachable by road (Metro Map of the city in the Info box gives exact location). Bengaluru is well connected by road, rail and air with the rest of the country and is also well known internationally.[8]

Gallery

  • Plaque declaring the Peninsular Gneiss as a Geological Monument
    Plaque declaring the Peninsular Gneiss as a Geological Monument
  • A plaque displayed at Lalbagh gives history of the tower and the garden
    A plaque displayed at Lalbagh gives history of the tower and the garden
  • Tourist at the Lalbagh Tower on the Peninsular Gneissic Rock hill
    Tourist at the Lalbagh Tower on the Peninsular Gneissic Rock hill

References

  1. ISSN 1432-1149
    .
  2. ^ a b c "Peninsular Gneiss". Geological Survey of India. Archived from the original on 21 July 2011. Retrieved 27 February 2009.
  3. ^
    ISSN 0254-0436
    .
  4. ^ a b "Lalbagh - Abounting with natural landmarks". Tourism Karnataka. Archived from the original on 5 January 2009. Retrieved 28 February 2009.
  5. ISBN 9780444415103
    .
  6. doi:10.1007/BF01830449
    .
  7. ^ "stratigraphy of Asia ( in Asia: The Precambrian )". Retrieved 28 February 2009.
  8. ^ a b "lalbagh Botanical garden Bangalore". Mysore Horticulturtal Society, Bangalore. Archived from the original on 17 February 2012. Retrieved 28 February 2009.
  9. ^ "Kempe Gowdas of Bengalooru (Bangalore)". Vokkaligara Parishat of America (VPA). Retrieved 28 February 2009.

External links

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