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Cardamom Hills

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Journal Article
Published: 01 March 2021
Jour. Geol. Soc. India (2021) 97 (3): 255–260.
...Swapnil Kumar Rai; Divya Prakash; Roopali Yadav; Srishti Jaiswal; R.S. Kumar; Chandra Kant Singh Abstract An infrequent occurrence of sapphirine from metapelite rocks of the Cardamom hills of South India has been reported. This report of sapphirine may not be the first from the Southern Granulite...
FIGURES
First thumbnail for: New Finding of Silica-deficient Sapphirine-bearing...
Second thumbnail for: New Finding of Silica-deficient Sapphirine-bearing...
Third thumbnail for: New Finding of Silica-deficient Sapphirine-bearing...
Journal Article
Published: 01 March 1954
Geological Magazine (1954) 91 (2): 89–101.
...J. B. Auden Abstract The geometric drainage patterns observed in three areas in India have led to closer study and the location of shatter zones that are considered the source of control. In the Cardamom hills area in south India the major control of drainage is the northwest-southeast strike...
Image
Geological map of the Southern Granulite terrane and the locations of the metasediments analyzed in this study (SZ—shear zone). WDC—western Dharwar craton; CDC—central Dharwar craton; EDC—eastern Dharwar craton; MM—Madras Massif; NH—Nilgiri Hills Massif; BR—Biligiri Rangan Hills Massif; KM—Kolli Malai Hills Massif; SH—Sheveroy Hills Massif; BSZ—Bhavani shear zone; PCSS—Palghat-Cauvery shear system; MO—Manamedu ophiolite complex (ca. 740–800 Ma); SA—Sittampundi ultramafic complex; AH—Anaimalai Hills Massif; KH—Kodaikanal Hills Massif; KD—Kadavur Dome; NMB—northern Madurai block; SMB—southern Madurai block; CH—Cardamom Hills Massif; TB—Trivandrum block; KKB—Kerala Khondalite Belt.
Published: 01 May 2014
—southern Madurai block; CH—Cardamom Hills Massif; TB—Trivandrum block; KKB—Kerala Khondalite Belt.
Image
Map of the Kerala Khondalite Belt (KKB), South India, showing locations of sample sites (circles labeled ED1–ED11) and main towns. Most sample sites and towns are near the Kozhencherry to Trivandrum Road (irregular line). Shaded and patterned areas refer to geological provinces or blocks as discussed in the text. Inset map shows the position of the KKB in relation to other geological domains and area of southern India. 1, Dhawar Craton, north of the orthopyroxene-in isograd. 2, Archean areas south of the orthopyroxene-in isograd. 3, Madurai Block and Kodaikanal–Cardamom Hills massifs (K-CHM). 4, Kerala Khondalite Belt (KKB). 5, Recent cover. NH, Nilgiri Hills; BSZ, Bhavani Shear Zone; PCSZ, Palghat-Cauvery Shear Zone.
Published: 01 November 2000
or blocks as discussed in the text. Inset map shows the position of the KKB in relation to other geological domains and area of southern India. 1 , Dhawar Craton, north of the orthopyroxene-in isograd. 2 , Archean areas south of the orthopyroxene-in isograd. 3 , Madurai Block and Kodaikanal–Cardamom
Journal Article
Published: 01 August 1989
Jour. Geol. Soc. India (1989) 34 (2): 147–151.
...D. C. Mishra; A. P. Singh; M. B. S. Vyaghreswara Rao Abstract The Idukki earthquake with epicentre around Nedumkandam, approximately 20 km east of the Tdukki reservoir, has been in the news. A detailed gravity profile from Bangalore to Trivandrum across Cardamom-Palni hill ranges has delineated...
Journal Article
Published: 01 January 1990
Jour. Geol. Soc. India (1990) 35 (1): 99–105.
... shows that the area comprises essentially of granites, granitic gneisses and migmatites. It has to be ascertained whether these granites represent a single emplacement or a number of plutonic bodies within the gneisses. -Cardamom hills domain The Cardamom hills domain, south of the Anamalai hills...
Journal Article
Published: 01 May 1993
Jour. Geol. Soc. India (1993) 41 (5): 431–436.
... the granulite province of southern Peninsular India consisting of high grade rnetamorphics, 0016 -7622/93/41-5-431/$ 1.OO 0 Geol. Soc. India. 432 N. K.THAKUR AND NANDINI NAGARAJAN granites and gneisses as exposed in the discontinuous hills of Palni-Cardamom and Anamalai as well as the pIains to the east...
Book Chapter

Author(s)
K. Soman
Series: Text Book
Published: 01 January 2023
DOI: 10.17491/bgsi.2023.986709
EISBN: 978-93-80998-67-1
...-mobile belts resulted in a large wedge of charnockite massif ( Fig.12 ) making up the Palni-Anaimalai-Cardamom hills ( Katz, 1978 ). The ‘Cardamom hill charnockite massif’, extending from the southern flank of the Palghat Gap and encompassing the eastern parts of Thrissur, Ernakulam and Kottayam...
Journal Article
Published: 01 September 1975
Jour. Geol. Soc. India (1975) 16 (3): 349–353.
... the east, King (1962) suggests a Gondwana cycle of planation for the remnants that now survive at elevations of 8760' (2633 m) and 8800' (2695 m) upon the Nilgiri and the Cardamom hills respectively; a Post-Gondwana cycle of landscape around 6500' (1969 m) near Ootacamund and some of the higher levels upon...
Journal Article
Published: 24 April 2017
Geological Magazine (2018) 155 (7): 1449–1464.
... not extend southeastwards paralleling the Thai–Cambodian border, nor extend under the Cardamom Mountains but, rather, extends eastwards into Cambodia and possibly then turns southwards along the strike of the Pursat–Kampot Fold Belt. Gubler ( 1935 ) mapped metamorphic and igneous rocks which he included...
FIGURES
First thumbnail for: Early Permian radiolarians from the extension of t...
Second thumbnail for: Early Permian radiolarians from the extension of t...
Third thumbnail for: Early Permian radiolarians from the extension of t...
Journal Article
Published: 01 November 2000
The Journal of Geology (2000) 108 (6): 687–703.
... or blocks as discussed in the text. Inset map shows the position of the KKB in relation to other geological domains and area of southern India. 1 , Dhawar Craton, north of the orthopyroxene-in isograd. 2 , Archean areas south of the orthopyroxene-in isograd. 3 , Madurai Block and Kodaikanal–Cardamom...
FIGURES
First thumbnail for: A Reappraisal of the Pressure-Temperature Path of ...
Second thumbnail for: A Reappraisal of the Pressure-Temperature Path of ...
Third thumbnail for: A Reappraisal of the Pressure-Temperature Path of ...
Image
(a) Simplified terrane map of mainland South East Asia with major terranes and sutures showing study area locations. BRS – Bentong–Raub Suture; CM – Chiangmai; DBF – Dien Bien Phu Fault; HN – Hainan Island; LPB – Luang Prabang; MPF – Mae Ping Fault; MYF – Mae Yuem Fault; NR – Nakhon Ratchasima (Khorat); PKF – Poko Fault Zone; S – Simao; TPF – Three Pagodas Fault; TPS – Tamky–Phuoc Son Suture; TKF – Thakhek Fault. (b) Diagrammatic map showing the three main postulated trends of the continuation of the Sa Kaeo Suture from or in SE Thailand into Cambodia from various authors. 1 – Paralleling the Thai–Cambodian border and following the imposed Indosinian Orogenic grain within Thailand (e.g. Arboit et al. 2016). 2 – Southeasterly trend beneath the Jurassic–Cretaceous terrestrial sandstones of the Cardamom Mountains in Cambodia (e.g. Qian et al. 2016; Sone, Metcalfe & Chaodumrong, 2012). 3 – Easterly trend following the northern margin of the Cardamom Mountains and then either continuing east (3ii) or trending south along the Pursat–Kampot Fold Belt (3i) (e.g. Khin Zaw et al. 2014). (c) Simplified compilation of relevant geology in eastern Thailand and western Cambodia. SE Thailand based on Hada et al. (1997), Chutakositkanon & Hisada (2008) and maps of the Geological Survey Bureau, Department of Mineral Resources, Bangkok. Western Cambodia geology is based on 1:500000 scale map of the Pak Nam sheet mapped by J. Gubler in 1935 with additional mapping by E. Saurin in 1962 for the Service Géologiques de l’Indochine and the 1:200000 BRGM map of the Pothisat sheet by Dottin & Zinszner (1972). Although originally regarded as Devonian, the Cambodian cherts are now, at least in part, reliably dated herein as Early Permian in age. By comparison with cherts in adjacent parts of Thailand, it is probable that both the cherts and the other sedimentary rocks near Pailin are also Permian. South of Pailin, the turbiditic sandstones are correlated with the Triassic submarine fan deposits of the Pong Nam Ron Formation. Point 1 – old abandoned quarries on eastern outskirts of Pailin; Point 2 – new, recently active, quarry to east of Pailin, lat. 12°49′51″N, long. 102°36′43.44″E, elevation 227 m; Point 3 – Phnom Kiaow, steeply dipping succession of shale/sandstone with poorly sorted sandstone-greywacke at top of hill, near waterfall at lat. 12°47′48.835″N, long. 102°36′56.270″E; Point 4 – Lower Permian radiolarian–conodont chert – basalt locality of Saesaengseerung et al. (2009) at Khao Phasuk (lat. 13°14′733″N, long. 102°13′807″E) in Thailand.
Published: 24 April 2017
– Paralleling the Thai–Cambodian border and following the imposed Indosinian Orogenic grain within Thailand (e.g. Arboit et al . 2016 ). 2 – Southeasterly trend beneath the Jurassic–Cretaceous terrestrial sandstones of the Cardamom Mountains in Cambodia (e.g. Qian et al . 2016 ; Sone, Metcalfe
Journal Article
Published: 01 January 1985
Jour. Geol. Soc. India (1985) 26 (1): 28–37.
... to the north of the Nilgiris and to the Kottai Malai (2018 m), the Devar Malai (1922 m) and the Agastya Malai (1869 m) in the Cardamom and the Varushanad hills to the south of the Palni hills. Reconstruction of the palaeosurface based on the remnants suggests that the surface marked by a physiographic high...
Journal Article
Published: 01 May 1978
Jour. Geol. Soc. India (1978) 19 (5): 185–205.
... of the Kerala aulacogene (Fig. 4). The Salem, Madurai and Kerala aulacogenes intersect to form the charnockitic massif of the Anamalai (AN)-Palni (PA)-Cardamom (CD) Hills. Sri Lankian Aulacogene The NE trending Highland Series of Sri Lanka is the best developed aulacogene of the region, with prominent lineament...
Journal Article
Published: 01 June 1968
Jour. Geol. Soc. India (1968) 9 (1): 67–74.
... to the seismic sketch map of India accompanying the above paper shows a marked concentration of epicentres along the east coast from Nellore to Ganjam, near Salem and its surroundings, the eastern margin of the Nilgiri and Cardamom hills, in south Travancore and the Central Highlands of Ceylon. The Count...
Journal Article
Published: 01 January 2001
Journal of Sedimentary Research (2001) 71 (1): 50–60.
... the Kaveri River. These two major tributaries also originate from the uplifted regions of Nilgiri, Cardamom, and Anaimalai hills. The two major tributaries and the main channel are thought to follow major, crustal-scale shear known as the Palghat-Kaveri gap, separating two continental blocks ( Radhakrishna...
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First thumbnail for: Geochemistry of the Floodplain Sediments of the Ka...
Second thumbnail for: Geochemistry of the Floodplain Sediments of the Ka...
Third thumbnail for: Geochemistry of the Floodplain Sediments of the Ka...
Journal Article
Published: 01 July 1995
Jour. Geol. Soc. India (1995) 46 (1): 37–45.
.... Metamorphic 0016-7622/95-46-1-37/$ l.OO©GEOL. SOc. INDIA D.V. SUBBA RAO AND OTHERS evolution and the nature of the provenance arc also discussed . GEOLOGICAL SETTING The Kodaikanal block comprtSlng Anaimalai, Palni and the Cardamom hills arc predominantly composed of orth ogenisses (charnocki te, basic...
Journal Article
Published: 01 January 1999
Jour. Geol. Soc. India (1999) 53 (1): 27–37.
... This valley has a distinct linear expression on the satellite mosaic of South India and forms an integral part of the SGT. It is bordered by the Kodaikatial hills in the north,the Cardamom hills in the west and Varushanad hills in the east (Fig.1). The valley is the geomorphicexpression of deep crustal fault...
Journal Article
Published: 01 October 2024
Jour. Geol. Soc. India (2024) 100 (10): 1443–1456.
... in the south, such as Nilgiris, Anamalais, Cardamom hills and Agasthyamalai range, it is referred to as Southern Block. The South Western Ghats cause moisture-filled winds from the Arabian Sea to rise, resulting in a heavy downpour of nearly 2000 mm per year. Downpours are more common in the south and last...
FIGURES
First thumbnail for: Landslides: A Review from the Southern Western Gha...
Second thumbnail for: Landslides: A Review from the Southern Western Gha...
Third thumbnail for: Landslides: A Review from the Southern Western Gha...
Book Chapter

Series: Text Book
Published: 01 January 2022
DOI: 10.17491/bgsi.2022.9858.03
EISBN: 9789380998589
... from west to east. The western part is marked by the Western Ghat hill ranges trending in a NNW-SSE direction from near Kanyakumari in the south through Kerala, Tamil Nadu and extends further northwards into Karnataka, Maharashtra and Goa. The elevation of the hills ranges between 1275 and 2637m...