-17- AN INTRODUCTORY STUDY OF THE MARINE ALGAL ECOLOGY OF AN OPEN COAST AREA AT LEIGH. by W. B. Silvester

Size: px
Start display at page:

Download "-17- AN INTRODUCTORY STUDY OF THE MARINE ALGAL ECOLOGY OF AN OPEN COAST AREA AT LEIGH. by W. B. Silvester"

Transcription

1 -17- AN INTRODUCTORY STUDY OF THE MARINE ALGAL ECOLOGY OF AN OPEN COAST AREA AT LEIGH by W. B. Silvester The supra-littoral, littoral and sub-littoral zonation of the open coast in the Leigh area are discussed. The communities are recognised and related to tide heights and exposure. LOCALITY Leigh is situated immediately south of Cape Rodney on the east coast of New Zealand, forty miles north of Auckland. A list of the algae to be found in Leigh Cove is given by Dellow (1955). The open coast ecology of the area immediately south of the Leigh inlet is discussed in this survey. GEOLOGY The rocks exposed in the area provide a striking contrast to the usual type of shore line in the Hauraki Gulf, which is sandstones and mudstones of the Waitemata series. The strata exposed on the Leigh coast however, belong to the Waipapa Group of Mesozoic age, consisting of indurated greywackes, sandstones, arid argillites. They differ from the West Coast sandstones of a comparable age in being considerably contorted and folded. The greywackes of this group outcrop on about six miles of coastline from Cape Rodney to the Tawharanui peninsula and are overlain with a cover of tertiary beds of the Waitemata Group. (Although most of the offshore islands of the Gulf consist largely of these greywackes, they do not outcrop on the mainland in any large quantity between Orere Point and Whangarei, Hopgood (1959) ). The hard and well weathered nature of the substratum exposed on the Leigh coast has a marked effect on both the zonation and the flora.

2 HAURAKI GULP PIG. I LOCALITY MAP

3 S I I 5 1MESEMBRYANTHEMUMAUSTRALE 1 SAMOLUS gggfgj ZZZ [LICHINA PYGMAEA MELARAPHE OLIVERI" "2 BOSTRYCHIA ARBUSCULA CHAMAESIPHO BRUNNEA CHAMAESIPHO COLUMNA 1 APOPHLOEA SINCLAIRII SAXOSTREA GLOMERATA POMATOCEROS COERULEUS J HORMOSIRA BANKSII "1 CORALLINA OFFICINALIS XIPHOPHORA CHONDROPHYLLA ~") CYSTOPHORA TORULOSA ] CARPOPHYLLUM MASCHALOCARPUM ECKLONIA RADIATA C/* ~o m Q m c/> > O o < m n > 2 I CO C O z O -n SAXOSTREA < GLOMERATA POMATOCEROS COERULEUS

4 -20- OBSERVATIONS The Leigh coast because of its position and due to the nature of the substratum, provides a marked contrast with conditions to be found in more sheltered parts of the Gulf. For these reasons, wherever possible, - comparisons are made between the two. Three features of general contrast are at once apparent. 1. Although the exposure is not nearly as great as that to be found on the West coast, Leigh, lacking the shelter of the Hauraki Gulf is exposed to the full force of most of East or N. E. winds. These at times send spray 20 and 30 ft. up the cliff faces. 2. As a result of the broken coastline, the large boulders and the deeply weathered substratum, conditions of light, wave action and wind vary greatly over relatively short distances. These factors produce a complex and diverse zonation. 3. The rock substratum differing as it does from the softer, more porous sandstones and mudstones of the Waitemata series supports an algal flora more comparable with that found on basalt. This is displayed at Leigh by the great profusion of Apophloea sinclairii which is found very rarely on Waitemata rocks but grows well on the basalt of Rangitoto. TIDE LEVELS The tidal range at Leigh was calculated as being 79% that of Auckland. Thus the vertical range of extreme spring tides at Leigh was estimated as 9. 6'. The EHWS and ELWS marks roughly corresponding to the 10' and 0. 4' levels respectively as measured from the Auckland Harbour Board datum of 0. 00'. The area was visited in summer, autumn and winter and changes were noted over these periods. Sampling was confined to the exposed area immediately below Leigh township. At this point a narrow headland or stack protrudes some fifty feet into the sea in a S. E. N. W. direction. Most of the sampling was done in and around this stack as it provided all degrees of exposure and shelter. Three transects were studied in varying degrees of exposure and compared with similar adjacent areas along the beach. The species present were classified as follows: - - dominant (a) - abundant - frequent

5 -21- (0) - occasional (r) - rare (1) - local The broad vertical distribution of species at Leigh falls into the same four groups as described by Stephenson (1939) for the Coast of South Africa and employed by Dellow (1950) and Carnahan (1952) in describing zonation within the Hauraki Gulf. These four zones are termed: (1) Littorina zone (2) Barnacle zone (3) Mixed Algal zone (4) Sublittoral fringe. The supra-littoral area at Leigh is also discussed. SUPRA-LITTORAL ZONE In sheltered and shady places plants of this zone extend down to within two feet of EHWS. Two separate associations are recognisable: ME TROSIDEROS - STIPA COMMUNITY Range: In the upper splash zone Metrosideros excelsa Stipa teretifolia Scirpus nodosus Astelia solanderi Apium pro stratum Peperomia urvilleana Asplenium flaccidum Asplenium lucidum (a) (a) HALOPHYTE COMMUNITY Range: From within two feet of EHWS upwards. Salicornia australis Mesembryanthemum australe Samolus repens Coprosma repens

6 -22- This very compact community forms dense mats on almost bare rock, excluding any subordinate species. Individual plants of Salicornia and Samolus grow in fissures near EHWS mark while the trailing stems of the other two members of the community extend well down the cliff faces. In its lower limits this association is admixed with a grey and yellow lichen community which extends into the supra-littoral fringe. LITTORINA ZONE This zone is characteristic of the upper littoral and lower supra-littoral. positions of maximum exposure or in shaded areas the zone is extended upwards. In MELARAPHE - LICHINA COMMUNITY: Range: MHWM to upper heavy spray limit Melaraphe oliveri Lichina pygmaea Nerita melanotragus Bostrychia arbuscula (1) Chamaesipho brunnea (1) Melaraphe may move over a wide area retreating into fissures well up in the supra-littoral. Where the dual action of shade and high spray are acting on the south faces this zone may be extended 10' above EHWS. On the north and East facing sides - where exposure is greatest - the wide storm platform and the drying effect of the sun tend to depress the upper limit of this community. Quantitatively this may be as much as a 3' depression. The vertical elevation of Melaraphe is considerably less than on the west coast but appreciably greater than that within the Gulf. Bostrychia and Chamaesipho are affected to a lesser degree. BOSTRYCHIA ARBUSCULA Range: EHWS and above - MHWS COMMUNITY: Bostrychia arbuscula Caloglossa leprieurii Lomentaria umbellata Cent roc eras clavulatum Polysiphonia sp. Rhizoclonium riparium Chamaesipho brunnea (1, f) Oscillatoria nigroviridis (r)

7 -23- Bostrychia forms a dense mat especially in moist shaded crevices. In more sheltered but sunny areas Caloglossa and Rhizoclonium tend to become abundant. Here again the large barnacle Chamaesipho brunnea may have a swash zone through this community. Lomentaria forms frequent tufts in the felt of Bostrychia. The major development of this community occurs above the barnacle zone but the two communities merge at the interface. ROCK POOL COMMUNITY: Range: Above MHWS Lyngbya maiuscula Lophosiphonia macra Derbesia novae-zealandiae The small rock pools on the platform support large tufts of Lyngbya and lesser amounts of Derbesia on the bare rock. Lophosiphonia characteristically grows on firm sand and its abundance increases with sedimentation. BARNACLE ZONE The communities of this zone occupy a wide portion of the mid-littoral area. The whole of the mid-littoral area is dominated by the two barnacles, the oyster and Apophloea, the latter two giving the shore a distinct white and red banded appearance. CHAMAESIPHO BRUNNEA Range: EHWS - MHWS COMMUNITY: Chamaesipho brunnea Bostrychia arbuscula Chamaesipho columna Nerita melanotragus This rather compact community occurs from just above to just below the wave cut platform on the stack. It is present infrequently on isolated boulders. The barnacle formation at Leigh of C. brunnea n'orming a distinct zone above C. columna is characteristic of exposed coast oceanic conditions, e. g. Great Barrier Island. Below the C. brunnea community and sharply divided from it there is a very wide mid-littoral zone. Although not dominated in all places this zone is at least characterised throughout by the small barnacle C. columna. The other two species which co-dominate in this zone viz. Apophloea sinclairii and Saxostrea glomerata are

8 -2Umuch more sensitive to exposure, and have narrower vertical ranges. For these reasons they are not found in every transect nor do they occur through the full range of Chamaesipho columna. The ranges for the three species are: C. columna MHWS - MLWN Apophloea MHWM - MLWN Saxostrea MHWN - E(H)LWN This community therefore occupies the wide vertical range of seven feet comprising 70% of the littoral zone at this station. The mid-littoral zone because of its position in the centre of the intertidal area, is exposed to wave action for more time than any other zone. Consequently, even though there are only three species occurring in abundance, a great diversity of zonation is found which does not allow them to be placed in circumscribed associations. At Leigh three grades of exposure can be observed both from observation of wind direction and exposure, and their correlation with the organisms. A. Very sheltered, in the lee of the stack among the boulders. B. Relatively sheltered, in the lee of the stack. C. Fully exposed, unsheltered by any rock formation. The barnacle zone is best studied under these three exposure conditions. A. Very sheltered. Apophloea sinclairii appears to demand the most sheltered environment of the three species and is therefore found to dominate at A. As Chamaesipho extends higher than Apophloea it forms a distinct band above it of about 6-9". Apophloea then dominates and forms a very compact consociation almost to the exclusion of the barnacle with which it obviously competes. On the sheltered but still sunny sides of the rocks Apophloea forms its characteristic erect portions. At about E(L)HWN the oyster Saxostrea begins to assume importance and below this at about MSL Apophloea and the oyster often form a compact association, but because of the very variable conditions among the rocks either may drop out. Below the lower limit of the oyster Apophloea and Chamaesipho are dominant according to conditions of light. Just below or partially obliterating this latter zone there may occur a thick mat of Pomatoceras coeruleus the spiny tube worm. These were found at A and C but not at B. B. Relatively sheltered As the exposure is increased Apophloea tends to be replaced at all heights by Chamaesipho. The amount of oyster coverage is diminished slightly but not to the same extent as the red alga. Consequently there appears a distinct Chamaesipho consociation above a Saxostrea - Chamaesipho association.

9 -25- C. Fully exposed At C, on the completely exposed side of the stack a further reduction in the oyster cover was noticed. This was correlated with a greater cover of barnacles which in this situation dominate throughout. Occasional molluscs found throughout the barnacle zone are Turbo (Lunella) smaragda, Nerita melanotragus, Cellana radians and Notoacmea pileopsis, and the white rock shell Neothais scalaris. The oyster borer Lepsiella scobina in places becomes quite frequent. Also found are Sypharochiton pelliserpentis, Onchidella patelloides, and Volsella neozealanicus. Occasional algae include Laurencia distichophylla, Gelidium caulacantheum and Scytothamnus australis. MIXED ALGAL ZONE This lower zone supports a wide variety of algae in the region from E(H)LWN to MLWS. The dominants of the area are also very sensitive to exposure effects and the composition of the zone varies greatly in the three degrees of exposure. Nevertheless four relatively distinct communities can be recognised. CORALLINA - HORMOSIRA Range: E(H)LWN - MLWS COMMUNITY: Corallina officinalis Hormosira banksii Jania hombroniana Ralfsia verrucosa Melobesia sp. Codium adhaerens Laurencia botrichioides Cellana radians Nerita melanotragus The two dominants are sensitive to exposure and occur in greatest abundance at A where Hormosira may grow quite large. At B there are small amounts of a stunted open coast form of Hormosira, while it is absent at C. Corallina with a smaller amount of Jania is able to survive exposure better and is found commonly at C. At A Ralfsia may form a definite zone just above the Hormosira and mixing in places with Apophloea. At B however it forms mats in positions that Hormosira would be expected to grow, while on smoother almost vertical rock both the Hormosira and Ralfsia are absent, leaving completely bare areas between the oyster zone above and Corallina below. The community is con-

10 -26- siderably compressed at C by a Melobesia community above and a fine algal turf below. The small amounts of Hormosira at B may be due to the almost vertical slope of the rock as well as to exposure. At C however, its absence is due purely to the greater exposure. In general Corallina assumes full dominance below Hormosira, but in some cases they may form two distinct zones. ENCRUSTING CORALLINE COMMUNITY: Range: E(H)LWN - ELWS Basal Corallina officinalis Melobesia sp. This community occurs only sparsely in the shelter at C, but it assumes an important position at B where the rock may be vertical and too steep for colonisation of other algae. On the exposed side of the stack it is important in depressing the zone of erect Corallina. In certain situations the community may extend down into the sub-littoral fringe. MIXED ALGAL TURF COMMUNITY: Range: MLWN - MLW Gelidium caulacantheum Caulacanthus spinellus Ulva lactuca Dictyota ocellata Champia novae-zealandiae Corallina officinalis Leathesia difformis Polysiphonia sp. Laurencia distichophylla Centroceras clavulatum (a) seasonal This community assumes importance only on the exposed side of the stack where it forms a distinct band mainly on the flatter rock immediately above the brown algal zone. It merges with Corallina above and Xiphophora below. Many subordinate species occur epiphytically in this turf, e. g. Pterosiphonia pinnata, Herposiphonia cerratoclada and Calithamnion sp. XIPHOPHORA - CYST OPHORA COMMUNITY: Range: MLWM - ELWS Xiphophora chondrophylla Cystophora torulosa

11 -27- These two brown algae form a distinct belt immediately above the sub-littoral fringe. They merge with the algal turf and Corallina zones above and with the Carpophyllums beneath-. Xiphophora is found growing in all transects while a distinct belt but it is hard to know whether the community lies in the sub-littoral fringe or in the mixed algal zone. They resemble the turf in being upright and relatively small compared with the large flaccid Carpophyllums and Ecklonia. On the other hand they are larger than all of the species of the turf and they are brown, giving them strong affinities with the sub-littoral fringe. Because of precedent I have included them in the mixed algal zone. SUB-LITTORAL FRINGE Again considerable variety within the one clearly defined zone can be seen. CARPOPHYLLUM - ECKLONIA COMMUNITY: Range: MLWS - below reach of all tides. Carpophyllum maschalocarpum Carpophyllum plumosum Ecklonia radiata Melanthalia abscissa Zonaria angustata Laurencia botrychioides Pterocladia capillacea Champia novae-zealandiae Liagora harveyana Laurencia distichophylla Lomentaria umbellata Tethya fissurata Rhodymenia leptophylla Glossophora kunthii (a) (a) (1, a) seasonal Epiphytic Metamorphe colensoi (a) Abroteia suborbicularis (a) Hymenena variolosa Strebocladia (a) Melobesia sp. Of the dominants C. maschalocarpum and Ecklonia occur at all points but C. plumosum is found only in shallow sheltered areas. At A and B C. plumosum forms

12 -23- a dense mat with C. maschalocarpum, it may go above it in transect A. The water. Zonaria is found sheltering among the mat of Carpophyllums at all points but Melanthalia is only found at C. Champia may grow epiphytically or terrestrially. The small orange sponge Tethya and the iridescent alga Rhodymenia are frequent in deep water. The five common epiphytes may form a very dense mat on the Carpophyllums, Metamorphe and Abroteia often forming a complete cover on the basal, more sheltered parts. SEASONAL CHANGES Liagora harveyana and Leathesia difformis form a thick turf on sheltered rocks during the summer but quickly disappear in autumn. The latter is commonly found at about MLWM while the former is at about ELWS in the summer months. FRESH WATER SEEPAGE In a region of fresh water seepage two species dominated, Chaetamorpha aerea and Enteromorpha intestinalis. EXPOSURE The three exposure transects studied reveal the following distributions: Species Transect A B C Apophloea sinclairii d o absent Saxostrea glomerata d f - d o Chamaesipho columna f - d d d Hormosira banksii d o absent Cystophora torulosa d d " Carpophyllum plumosum d d " Melanthalia abscissa absent absent f These results may reflect variations in the slope of the rock, sun and shade as

13 -29- well as exposure. LEVELLING SURVEY A levelling survey was carried out for the dominant and physiognomically important species occurring in the area. As has been previously demonstrated for other areas Dellow (1950), Beveridge and Chapman (1950) and Carnahan (1952) four critical levels are seen. I II m IV Between MHWS and MHW Between E(H)LWN and MLWN At approximately MLW, this is perhaps not a valid critical level. Between MLWS and ELWS. These limits show graphically the basis on which the littoral area is divided into its four zones. SUMMARY The communities are described as far as possible for the open coast at Leigh and their tide heights in relation to the A. H. BJD. are given. Comparisons are drawn with stations deeper in the Hauraki Gulf as to exposure and rock type and their subsequent effects on zonation. Three transects were made and from these, three types of exposure are discussed in relation to the zonation of particular communities and species. It is recognised that to gain a fuller picture of the area a deeper and more concentrated study should be made over a wider period of time. The Leigh coast provides an ideal area in which the differential effects of exposure, shade, rock type and slope can be studied. Further work on these lines should prove very rewarding. ACKNOWLEDGEMENTS The writer wishes to acknowledge the help given by Mr D. J. Chapman in identifying many of the algal specimens, to Professor V. J. Chapman under whom the study was made and to Miss J. Wheeler for the use of her unpublished notes on Apophloea sinclairii.

14 -30- APPENDIX I Algal species found in the area and not listed in the text are given below. Ulva parva Enteromorpha bulbosa Cladophora crinalis Cladophoropsis herpestica Bryopsis plumosa Lola tortuosa Chaetamorpha melargonium Notheia anomala Bangia fusco-purpurea Porphyra columbina Gelidium pusillum Antithamnion sp. Callithamnion sp. Laurencia virgata Herposiphonia cerratoclada Pterosiphonia pinnata Euzoniella sp. REFERENCES Batham, E. J Ecology of Southern New Zealand Sheltered Rocky Shore. Trans. Roy. Soc. N. Z. Vol. 84, Pt. 2, Ecology of Southern New Zealand Exposed Rocky Shore at Little Papanui, Otago Peninsula. Ibid. Vol. 85, Pt. 4, pp Beveridge, W. A. & Chapman, V. J The Zonation of Marine Algae at Piha, in relation to the Tidal Factor. Pacific Science, Vol. 4, pp Carnahan, J. A. Chapman, V. J Intertidal Zonation at Rangitoto Island, New Zealand. Pacific Science, Vol. 6, pp The Marine Algal Communities of Stanmore, Bay, New Zealand. Pacific Science, Vol. 4, pp

15 -31- Chapman, V. J. Dellow, V. Dell, R. K. Hopgood, A. M. Lindauer, V. W. Moore, L. B., Stephenson, T. A. Trevarthan, C. B The Marine Alga of N. Z. Pt. 1, Myxophyceae and Chlorophyceae. Journ. of the Linn. Soc. Lond. Botany. Vol. LV. No pp Intertidal Ecology at Narrow Neck Reef, New Zealand. Pacific Science, Vol. 4, pp Marine Algal Ecology of the Hauraki Gulf, New Zealand. Trans. Roy. Soc. N. Z., Vol. 83, Pt. I, pp Native Shells Notes on the Structure of Greywackes and Argillites at Tawharanui Peninsula, Auckland. N. Z. Journ. of Geo, and Geophysics, Vol. 3, No. 2, pp A Descriptive Review of the Phaeophyceae of N. Z. Trans. Roy. Soc. N. Z., Vol. 85, Pt. 1, pp Some intertidal Sessile Barnacles of N. Z. Soc. N. Z., Vol. 73, pp Trans. Rov "Our Living Environment" - Seaweeds. Post Primary Schools Bulletin, Vol. 2, No. 13, Wellington The Constitution of the Intertidal Fauna and Flora of South Africa, Pt. 1, Linn. Soc. Lond. Journ. Zool., Vol. 40, pp The Use of A Zonation Diagram in Intertidal Ecology Science Record, Dunedin, Vol. 3, pp

SOME FACTORS AFFECTING ZONATION OF ROCKY SHORE ORGANISMS AT KAWERUA. by B.W. Hayward *

SOME FACTORS AFFECTING ZONATION OF ROCKY SHORE ORGANISMS AT KAWERUA. by B.W. Hayward * Tane (1971) 17:137-148 137 SOME FACTORS AFFECTING ZONATION OF ROCKY SHORE ORGANISMS AT KAWERUA by B.W. Hayward * SUMMARY The zonation patterns of the rocky shore organisms at Kawerua, on the west coast

More information

T H E E C O L O G Y O F T H E SUB L I T T O R A L B O U L D E R B E A C H E S A T L I T T L E B A R R I E R ISLAND. by F. I. Dromgoole.

T H E E C O L O G Y O F T H E SUB L I T T O R A L B O U L D E R B E A C H E S A T L I T T L E B A R R I E R ISLAND. by F. I. Dromgoole. 70. T H E E C O L O G Y O F T H E SUB L I T T O R A L B O U L D E R B E A C H E S A T L I T T L E B A R R I E R ISLAND by F. I. Dromgoole. A B S T R A C T The sublittoral ecology at three localities on

More information

by B.A. Foster THE EFFECT OF ASPECT ON POPULATION COMPOSITION

by B.A. Foster THE EFFECT OF ASPECT ON POPULATION COMPOSITION TANE (1966) 12 : 37-44 37 THE EFFECTS OF WAVE EXPOSURE AND ASPECT ON THE VERTICAL SHORE DISTRIBUTION AND POPULATION COMPOSITION OF MELARHAPHA OLIVERI. by B.A. Foster INTRODUCTION The periwinkle Melarhapha

More information

THE INTERTIDAL LIFE OF RUAMAHUA-ITI AND MIDDLE ISLAND (ALDERMEN ISLANDS) by Anne B. Saies* SUMMARY

THE INTERTIDAL LIFE OF RUAMAHUA-ITI AND MIDDLE ISLAND (ALDERMEN ISLANDS) by Anne B. Saies* SUMMARY I THE INTERTIDAL LIFE OF RUAMAHUA-ITI AND MIDDLE ISLAND (ALDERMEN ISLANDS) by Anne B. Saies* SUMMARY The distribution of intertidal organisms of Ruamahua-iti and Middle Island, two islands of the Aldermen

More information

Removal of intertidal algae by herbivores in experimental frames and on shores near Auckland

Removal of intertidal algae by herbivores in experimental frames and on shores near Auckland New Zealand Journal of Marine and Freshwater Research ISSN: 0028-8330 (Print) 1175-8805 (Online) Journal homepage: https://www.tandfonline.com/loi/tnzm20 Removal of intertidal algae by herbivores in experimental

More information

Competition and intertidal zonation of barnacles at Leigh, New Zealand

Competition and intertidal zonation of barnacles at Leigh, New Zealand New Zealand Journal of Marine and Freshwater Research ISSN: 0028-8330 (Print) 1175-8805 (Online) Journal homepage: http://www.tandfonline.com/loi/tnzm20 Competition and intertidal zonation of barnacles

More information

Types of intertidal communities

Types of intertidal communities Between the tides Marine ecosystems 1 Intertidal Delimited by the highest high tide and the lowest low tides marks The best studied and best-understood by humans Relatively easy to sample compared to other

More information

Black Point & Bihler Point

Black Point & Bihler Point Black Point & Bihler Point Conglomerate Photo: looking north toward end of Black Point (south of post 1) All of the rocks in this photo are conglomerate. Both Black Point and Bihler Point are formed from

More information

Geoduck Floating Nursery Monitoring Plan, Quarterly Reporting

Geoduck Floating Nursery Monitoring Plan, Quarterly Reporting December 23, 2014 Mason County Department of Community Development Attn: Grace Miller, Senior Planner 411 N. Fifth Street PO Box 279 Shelton, WA 98584 Re: Geoduck Floating Nursery Monitoring Plan, Quarterly

More information

Relatively little hard substrate occurs naturally in the

Relatively little hard substrate occurs naturally in the CHAPTER FIVE Rock Habitats Relatively little hard substrate occurs naturally in the estuary, owing mainly to the vast quantities of fine sediment that have been deposited by the rivers. Rock habitat is

More information

Depositional Environment

Depositional Environment Depositional Environment Sedimentary depositional environment describes the combination of physical, chemical and biological processes associated with the deposition of a particular type of sediment. Types

More information

Chapter 17. Ocean and Coastal Processes

Chapter 17. Ocean and Coastal Processes Chapter 17 Ocean and Coastal Processes Ocean Basins and Plates Ocean Basins Ocean Basins are profoundly different from the continents. Ocean crust is thin and dense and young. New ocean crust is generated

More information

Ocean and Coastal Processes. Ocean Basins. Chapter 20. Ocean Basins and Plates. Ocean Terms. Sea Arch Bay-mouth Bar Spit Tombolo Coast.

Ocean and Coastal Processes. Ocean Basins. Chapter 20. Ocean Basins and Plates. Ocean Terms. Sea Arch Bay-mouth Bar Spit Tombolo Coast. Chapter 20 Ocean Basins and Plates Ocean and Coastal Processes Tide Wave Height Length Period Base Refraction Tsunami Beach Sea stack Ocean Terms Sea Arch Bay-mouth Bar Spit Tombolo Coast Emergent Submergent

More information

The Coast: Beaches and Shoreline Processes Trujillo & Thurman, Chapter 10

The Coast: Beaches and Shoreline Processes Trujillo & Thurman, Chapter 10 The Coast: es and Shoreline Processes Trujillo & Thurman, Chapter 10 Oceanography 101 Chapter Objectives Recognize the various landforms characteristic of beaches and coastal regions. Identify seasonal

More information

The Coast: Beaches and Shoreline Processes

The Coast: Beaches and Shoreline Processes 1 2 3 4 5 6 7 8 9 The Coast: es and Shoreline Processes Trujillo & Thurman, Chapter 10 Oceanography 101 Chapter Objectives Recognize the various landforms characteristic of beaches and coastal regions.

More information

Significant Ecological Marine Area Assessment Sheet

Significant Ecological Marine Area Assessment Sheet Significant Ecological arine Area Assessment Sheet Name: Eastern Bay of Island Biogenic Soft Sediment Complex Summary: The semi-sheltered areas between the central islands of the Eastern Bay of Islands

More information

The Marine Environment

The Marine Environment The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write or. 1.

More information

GLY Coastal Geomorphology Notes

GLY Coastal Geomorphology Notes GLY 4734 - Coastal Geomorphology Notes Dr. Peter N. Adams Spring 2011 2 Coastal Classification In this lecture, we discuss some successful classification schemes of the coastal landscape, and pay particular

More information

Weathering of Rocks. Weathering - Breakdown of rocks into pieces (sediment) 2 main types of weathering to rocks

Weathering of Rocks. Weathering - Breakdown of rocks into pieces (sediment) 2 main types of weathering to rocks Weathering of Rocks Weathering - Breakdown of rocks into pieces (sediment) 2 main types of weathering to rocks Mechanical weathering requires physical forces to break rocks into smaller pieces. Chemical

More information

Subduction Zone Observatory

Subduction Zone Observatory Subduction Zone Observatory Observations made with simple tools can provide important scientific constraints. (can also combine with more sophisticated measurements). Standardized well-planned marine intertidal

More information

Australian Coastal Councils Conference

Australian Coastal Councils Conference Australian Coastal Councils Conference 11 March 2015 Estimating Future Coastal Inundation and Erosion Hazards Dr Andrew McCowan Dr Christine Lauchlan-Arrowsmith Warwick Bishop Background Victorian Future

More information

UNIT 1: WATER SYSTEMS ON EARTH CHAPTER 2: OCEANS CONTROL THE WATER CYCLE

UNIT 1: WATER SYSTEMS ON EARTH CHAPTER 2: OCEANS CONTROL THE WATER CYCLE UNIT 1: WATER SYSTEMS ON EARTH CHAPTER 2: OCEANS CONTROL THE WATER CYCLE ORIGINS OF OCEAN WATER OCEANS HAVE FILLED OVER HUNDREDS OF MILLIONS OF YEARS SCIENTISTS BELIEVE THE OCEANS ARE MORE THAN 3 BILLION

More information

Monitoring Marine Habitats of West Mainland Orkney: will Wave Energy Extraction contribute to long-term change?

Monitoring Marine Habitats of West Mainland Orkney: will Wave Energy Extraction contribute to long-term change? Monitoring Marine Habitats of West Mainland Orkney: will Wave Energy Extraction contribute to long-term change? Andrew Want Research Associate ICIT Heriot-Watt University Monitoring Marine Habitats of

More information

In 1990, 50% of the U.S. population lived within 75 km of a coast. By 2010, 75% of the U.S. population will live within 75 km of a coast.

In 1990, 50% of the U.S. population lived within 75 km of a coast. By 2010, 75% of the U.S. population will live within 75 km of a coast. In 1990, 50% of the U.S. population lived within 75 km of a coast. By 2010, 75% of the U.S. population will live within 75 km of a coast. High Tech Methods for Surveying the Deep Sea Floor Fig. 20.18 1

More information

COASTLINES MARINE EROSION PROCESSES. Read the course booklet.

COASTLINES MARINE EROSION PROCESSES. Read the course booklet. MARINE EROSION Read the course booklet. PROCESSES. You will need to know and be able to explain the four methods of coastal erosion and two of weathering The next few slides illustrate these processes.

More information

Phillip Island Nature Parks Coastal Process Study 8 October 2014

Phillip Island Nature Parks Coastal Process Study 8 October 2014 Phillip Island Nature Parks Coastal Process Study 8 October 2014 Project Overview Coastal Geology Basaltic and fragmented lavas, granite at Pyramid Rock and Cape Woolamai Weathered basalt (>10m thick)

More information

The Marine Environment

The Marine Environment The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write true or

More information

A SURVEY OF MARINE HABITATS AT KAWERUA. by Peter K-Dickson University of Auckland Marine Laboratory, R.D. Leigh. SUMMARY

A SURVEY OF MARINE HABITATS AT KAWERUA. by Peter K-Dickson University of Auckland Marine Laboratory, R.D. Leigh. SUMMARY A SURVEY OF MARINE HABITATS AT KAWERUA. by Peter K-Dickson University of Auckland Marine Laboratory, R.D. Leigh. SUMMARY A rocky subtidal area of Northland's west coast was studied using SCUBA. Results

More information

TI POINT BASALT INTRUSIVE OR EXTRUSIVE? Bruce W. Hayward

TI POINT BASALT INTRUSIVE OR EXTRUSIVE? Bruce W. Hayward TI POINT BASALT INTRUSIVE OR EXTRUSIVE? Bruce W. Hayward Auckland Geology Club has had two field trips to Ti Pt (in 2004 and 2012) to look at the Miocene basalt exposures and seek to determine whether

More information

1. Oceans. Example 2. oxygen.

1. Oceans. Example 2. oxygen. 1. Oceans a) Basic facts: There are five oceans on earth, making up about 72% of the planet s surface and holding 97% of the hydrosphere. Oceans supply the planet with most of its oxygen, play a vital

More information

Rocky Intertidal Ecology -- part II The development of experimental ecology. Connell and the experimental revolution

Rocky Intertidal Ecology -- part II The development of experimental ecology. Connell and the experimental revolution Rocky Intertidal Ecology -- part II The development of experimental ecology I. Intertidal Zonation, part II 1. Follow ups on Connell 2. Predation 3. Exceptions II. Horizontal Distribution 1. Variation

More information

Geol 117 Lecture 18 Beaches & Coastlines. I. Types of Coastlines A. Definition:

Geol 117 Lecture 18 Beaches & Coastlines. I. Types of Coastlines A. Definition: I. Types of Coastlines A. Definition: 1. Shore = narrow zone where ocean meets land (e.g. beach) 2. Coast is a broad area where both ocean and land processes act a. Includes onshore marshes, dunes, sea

More information

Introduction. The seashore. Tides

Introduction. The seashore. Tides Introduction The seashore One of the most striking features of the shore is the rich diversity of plant and animal life to be found there. A wide range of invertebrates, some highly mobile, others fixed

More information

Glacial Geology of Moose Point State Park, ME

Glacial Geology of Moose Point State Park, ME Geologic Site of the Month May, 2013 Glacial Geology of Moose Point State Park, Maine 44 o 25 59.18"N, 68 o 56 37.11"W Text and photos by Woodrow B. Thompson, Department of Agriculture, Conservation &

More information

What is weathering and how does it change Earth s surface? Answer the question using

What is weathering and how does it change Earth s surface? Answer the question using 7 th Grade Lesson What is weathering and how does it change Earth s surface? Answer the question using the sentence frame. You have 4 minutes. Weathering is. This changes the Earth s surface because. 1

More information

Spatiotemporal variations of hermit crab (crustacea: decapoda) inhabiting rocky shore along Saurashtra coast, western coast of India

Spatiotemporal variations of hermit crab (crustacea: decapoda) inhabiting rocky shore along Saurashtra coast, western coast of India Indian Journal of Geo-Marine Sciences Vol. 41 (2), April 2012, pp. 146-151 Spatiotemporal variations of hermit crab (crustacea: decapoda) inhabiting rocky shore along Saurashtra coast, western coast of

More information

CHAPTER 28. PHYSIOGRAPHY Cook Inlet Drainages

CHAPTER 28. PHYSIOGRAPHY Cook Inlet Drainages PEBBLE PROJECT ENVIRONMENTAL BASELINE DOCUMENT 2004 through 2008 CHAPTER 28. PHYSIOGRAPHY Cook Inlet Drainages PREPARED BY: Knight Piésold Ltd. PHYSIOGRAPHY COOK INLET DRAINAGES TABLE OF CONTENTS TABLE

More information

A NOTE ON LICHENS FROM RUAMAHUA-ITI, ALDERMEN ISLANDS. by B.W. Hayward* SUMMARY

A NOTE ON LICHENS FROM RUAMAHUA-ITI, ALDERMEN ISLANDS. by B.W. Hayward* SUMMARY 87 A NOTE ON LICHENS FROM RUAMAHUA-ITI, ALDERMEN ISLANDS by B.W. Hayward* SUMMARY Thirty-five lichen species from twenty genera are recorded from Ruamahuaiti, Aldermen Islands. A description of the lichen

More information

TECHNIQUES FOR ASSESSING COASTAL HAZARD AREAS FOR THE GISBORNE DISTRICT COAST

TECHNIQUES FOR ASSESSING COASTAL HAZARD AREAS FOR THE GISBORNE DISTRICT COAST TECHNIQUES FOR ASSESSING COASTAL HAZARD AREAS FOR THE GISBORNE DISTRICT COAST July 1994 C.R. 1994/12 Jeremy G Gibb 2009 All rights reserved. This work is entitled to the full protection given by the Copyright

More information

WELCOME TO ST ANDREWS ON TOUR: ORIELTON 2017

WELCOME TO ST ANDREWS ON TOUR: ORIELTON 2017 WELCOME TO ST ANDREWS ON TOUR: ORIELTON 2017 STAFF ANDY BLIGHT (Capt) SAFETY Signature! GRANT BROWN JEFF GRAVES GINNY GREENWAY SUE HEALY FAITH JONES DAVID PATERSON DAVID SHUKER Intertidal ecology: The

More information

All the soils are azonal, - immature and poorly developed.

All the soils are azonal, - immature and poorly developed. -45- VEGETATION TRANSECTS IN RANGITOTO CRATER By.. Lidgard INTRODUCTION Among the many volcanic cones of Auckland, Rangitoto, the most recent, still bears a complete and naturally developed plant cover.

More information

A SURVEY OF THE WESTERN BLUE GROPER IN WESTERN SOUTH AUSTRALIA

A SURVEY OF THE WESTERN BLUE GROPER IN WESTERN SOUTH AUSTRALIA A SURVEY OF THE WESTERN BLUE GROPER IN WESTERN SOUTH AUSTRALIA By Scoresby A. Shepherd and James B. Brook Reef Watch, c/o Conservation Council of South Australia, 120 Wakefield St, Adelaide, 5000. 4 January

More information

Supplemental Slides. Shore: Junction of Land & Water. Junction of Land & Water. Sea Level Variations. Shore vs. Coast. Sea Level Variations

Supplemental Slides. Shore: Junction of Land & Water. Junction of Land & Water. Sea Level Variations. Shore vs. Coast. Sea Level Variations Shore: Junction of Land & Water Supplemental Slides Sediments come off land Most get dumped at the beach Sediment interacts with ocean waves and currents Junction of Land & Water Features: Breaking waves,

More information

Shore: Junction of Land & Water. Sediments come off land Most get dumped at the beach Sediment interacts with ocean waves and currents

Shore: Junction of Land & Water. Sediments come off land Most get dumped at the beach Sediment interacts with ocean waves and currents Shore: Junction of Land & Water Supplemental Slides Sediments come off land Most get dumped at the beach Sediment interacts with ocean waves and currents Junction of Land & Water Features: Breaking waves,

More information

Paleo Lab #4 - Sedimentary Environments

Paleo Lab #4 - Sedimentary Environments Paleo Lab #4 - Sedimentary Environments page - 1. CHARACTERISTICS OF SEDIMENT Grain size and grain shape: The sizes and shapes of sedimentary particles (grains) are modified considerably during their transportation

More information

THE COASTAL GEOLOGY OF THE I HUM AT AO AREA, AUCKLAND

THE COASTAL GEOLOGY OF THE I HUM AT AO AREA, AUCKLAND TANE 23, 1977 THE COASTAL GEOLOGY OF THE I HUM AT AO AREA, AUCKLAND by B.D. Ricketts Department of Geology, University of Auckland, Private Bag, Auckland (Present address: Geology Department, Carleton

More information

2.2.7 Backbarrier flats

2.2.7 Backbarrier flats FIGURE 24. VERTICAL PHOTOGRAPH SHOWING THE DEVELOPMENT OF SMALL PARABOLIC DUNES FROM BLOWOUTS IN A LARGE RELICT FOREDUNE NORTHWEST OF HUNTER'S CREEK. PHOTOGRAPH COURTESY OF CAR'T'ER HOLT HARVEY FORESTS

More information

MIOCENE STRATIGRAPHY OF THE HOKIANGA - WAIMAMAKU COASTLINE, NORTH OF KAWERUA, NORTH AUCKLAND. by B.W. Hayward* SUMMARY

MIOCENE STRATIGRAPHY OF THE HOKIANGA - WAIMAMAKU COASTLINE, NORTH OF KAWERUA, NORTH AUCKLAND. by B.W. Hayward* SUMMARY 119 MIOCENE STRATIGRAPHY OF THE HOKIANGA - WAIMAMAKU COASTLINE, NORTH OF KAWERUA, NORTH AUCKLAND by B.W. Hayward* SUMMARY The lower Miocene geology of the 8 km coastal strip from Hokianga South Head to

More information

Oceanography. Oceanography is the study of the deep sea and shallow coastal oceans.

Oceanography. Oceanography is the study of the deep sea and shallow coastal oceans. Oceanography Oceanography is the study of the deep sea and shallow coastal oceans. Studying the Ocean Floor To determine the shape and composition of the ocean floor, scientists use techniques such as

More information

LAB 6: TRINIDAD BEACH FIELD TRIP

LAB 6: TRINIDAD BEACH FIELD TRIP OBJECTIVES: LAB 6: TRINIDAD BEACH FIELD TRIP 1) to develop your powers of observation, especially of geological phenomena; 2) to identify the rocks exposed at Trinidad Beach; 3) to reconstruct some of

More information

Florida Panhandle and Alabama Beaches Welcome Spring Break: Free of Tar Balls at Last

Florida Panhandle and Alabama Beaches Welcome Spring Break: Free of Tar Balls at Last Florida Panhandle and Alabama Beaches Welcome Spring Break: Free of Tar Balls at Last Ping Wang, James H. Kirby III, and Jun Cheng Coastal Research Laboratory, Department of Geology, University of South

More information

Environmental Science

Environmental Science Environmental Science A Study of Interrelationships Cui Jiansheng Hebei University of Science and Technology CH06 Kinds of Ecosystems and Communities Chapter Objectives After reading this chapter, you

More information

WHAT CAN MAPS TELL US ABOUT THE GEOGRAPHY OF ANCIENT GREECE? MAP TYPE 1: CLIMATE MAPS

WHAT CAN MAPS TELL US ABOUT THE GEOGRAPHY OF ANCIENT GREECE? MAP TYPE 1: CLIMATE MAPS WHAT CAN MAPS TELL US ABOUT THE GEOGRAPHY OF ANCIENT GREECE? MAP TYPE 1: CLIMATE MAPS MAP TYPE 2: PHYSICAL AND/OR TOPOGRAPHICAL MAPS MAP TYPE 3: POLITICAL MAPS TYPE 4: RESOURCE & TRADE MAPS Descriptions

More information

Larvae survive, grow, develop, disperse. Juvenile. Adult. Bipartite life cycle of benthic marine organisms with pelagic larvae. Pelagic Environment

Larvae survive, grow, develop, disperse. Juvenile. Adult. Bipartite life cycle of benthic marine organisms with pelagic larvae. Pelagic Environment Bipartite life cycle of benthic marine organisms with pelagic larvae Larvae survive, grow, develop, disperse Rocky Intertidal Pattern: species distributed in discrete zones relative to elevation and tidal

More information

Holocene evolution of Dahab coastline Gulf of Aqaba, Sinai Peninsula, Egypt 1

Holocene evolution of Dahab coastline Gulf of Aqaba, Sinai Peninsula, Egypt 1 Holocene evolution of Dahab coastline Gulf of Aqaba, Sinai Peninsula, Egypt 1 Magdy Torab* 2 * Prof. of Geomorphology, Department of Geography, Damanhour University, Egypt 3 E-mail: magdytorab@hotmail.com.

More information

Module 10: Resources and Virginia Geology Topic 4 Content: Virginia Geology Notes

Module 10: Resources and Virginia Geology Topic 4 Content: Virginia Geology Notes Virginia is composed of a very diverse landscape that extends from the beaches and barrier islands all of the way to the highly elevated Appalachian Plateau. Geologists have discovered ancient shallow

More information

Larvae survive, grow, develop, disperse. Adult. Juvenile. Bipartite life cycle of benthic marine organisms with pelagic larvae. Pelagic Environment

Larvae survive, grow, develop, disperse. Adult. Juvenile. Bipartite life cycle of benthic marine organisms with pelagic larvae. Pelagic Environment Bipartite life cycle of benthic marine organisms with pelagic larvae Larvae survive, grow, develop, disperse In the beginning when ecologists first wandered into the intertidal I. Pattern: species distributed

More information

Map 4: Cowal Peninsula: Cluniter to Ardyne Point Map Content Descriptions

Map 4: Cowal Peninsula: Cluniter to Ardyne Point Map Content Descriptions Map 4: Cowal Peninsula: Cluniter to Ardyne Point Map Content Descriptions 1. Built Heritage and Archaeology A total of twenty four sites were recorded in the area covered by Map 4. Of these six were previously

More information

Bipartite life cycle of benthic marine organisms with pelagic larvae. Larvae. survive, grow, develop, disperse. Pelagic Environment

Bipartite life cycle of benthic marine organisms with pelagic larvae. Larvae. survive, grow, develop, disperse. Pelagic Environment Bipartite life cycle of benthic marine organisms with pelagic larvae Larvae survive, grow, develop, disperse reproduce Pelagic Environment Benthic Environment settlement Adult Juvenile survive, grow, mature

More information

Percentage of normal rainfall for April 2018 Departure from average air temperature for April 2018

Percentage of normal rainfall for April 2018 Departure from average air temperature for April 2018 New Zealand Climate Update No 227, May 2018 Current climate April 2018 Overall, April 2018 was characterised by lower pressure than normal over and to the southeast of New Zealand. Unlike the first three

More information

Explained by Dr CJC Rees (York)

Explained by Dr CJC Rees (York) HOW THE TIDES WORK Explained by Dr CJC Rees (York) TIDES AND WATER MARKS TIDES and the - SYSTEM The earth-moon system rotates in space about its common centre of mass, there being a stabilising balance

More information

Coastal Erosion Landforms on the Gower Peninsula

Coastal Erosion Landforms on the Gower Peninsula Geo Factsheet www.curriculum-press.co.uk Number 356 Coastal Erosion Landforms on the Gower Peninsula The Gower The rocky southern coast of the Gower Peninsula in South Wales is home to long stretches of

More information

Shorelines and Diesel

Shorelines and Diesel Shorelines and Diesel Rock Platforms (bedrock): A common shoreline type with a rocky environment that is both exposed and submerged from tide cycles. Platforms are generally horizontal and collect sediments

More information

Science 8 - Water Systems Test - Chapters 1-2

Science 8 - Water Systems Test - Chapters 1-2 Science 8 - Water Systems Test - Chapters 1-2 Multiple Choice (30 marks) Identify the choice that best completes the statement or answers the question. 1. What percentage represents the amount of fresh

More information

Beach Pebbles Tell a Story

Beach Pebbles Tell a Story Maine Geologic Facts and Localities September, 2000 Text by Joseph T. Kelley, Department of Agriculture, Conservation & Forestry 1 Introduction The smooth, sandy beaches of southern Maine are popular with

More information

Hurricane Wilma Post Storm Data Acquisition Estimated Peak Wind Analysis and Storm Tide Data. December 27, 2005

Hurricane Wilma Post Storm Data Acquisition Estimated Peak Wind Analysis and Storm Tide Data. December 27, 2005 Hurricane Wilma Post Storm Data Acquisition Estimated Peak Wind Analysis and Storm Tide Data December 27, 2005 Hurricane Wilma was the sixth major hurricane of the record-breaking 2005 Atlantic hurricane

More information

NAME: GEL 109 Final Winter 2010

NAME: GEL 109 Final Winter 2010 GEL 109 Final Winter 2010 1. The following stratigraphic sections represents a single event followed by the slow accumulation of background sedimentation of shale. Describe the flows that produced the

More information

Effects of patch shape in intertidal algal mosaics: roles of area, perimeter and distance from edge

Effects of patch shape in intertidal algal mosaics: roles of area, perimeter and distance from edge Marine Biology (2003) 143: 639 650 DOI 10.1007/s00227-003-1119-3 L. Airoldi Effects of patch shape in intertidal algal mosaics: roles of area, perimeter and distance from edge Received: 20 November 2002

More information

Coastal Study Delimara Peninsula

Coastal Study Delimara Peninsula Coastal Study Delimara Peninsula Edward Gilson Fieldwork Report Coastal Study Coastal Processes Delimara Peninsula Location:. Date: Time:. Apparatus:. Weather Conditions: Objectives / Aims: Geography Option

More information

Jasper Beach, Machiasport, Maine

Jasper Beach, Machiasport, Maine Maine Geologic Facts and Localities June, 2000 Jasper Beach, Machiasport, Maine 44 o 38 30.28 N, 67 o 22 31.96 W Text by Joesph T. Kelley, Department of Agriculture, Conservation & Forestry 1 Map by USGS

More information

The Giant Tides of Fundy What are tides?

The Giant Tides of Fundy What are tides? The Giant Tides of Fundy What are tides? The tide is the natural change in elevation of water over time and can easily be observed along any ocean coastline. Some areas of the world have one high tide

More information

Shoreline and Climate Change Adaptation Alternatives for The Letter Parcel, Bolinas Lagoon

Shoreline and Climate Change Adaptation Alternatives for The Letter Parcel, Bolinas Lagoon Shoreline and Climate Change Adaptation Alternatives for The Letter Parcel, Bolinas Lagoon Scenic shoreline vista of Bolinas Lagoon and ridges, from Letter Parcel, March 2016 Peter Baye, Coastal Ecologist

More information

Subtidal permanently flooded with tidal water. Irregularly exposed surface exposed by tides less often than daily

Subtidal permanently flooded with tidal water. Irregularly exposed surface exposed by tides less often than daily Types of Wetlands Tidal Systems COASTAL WETLAND ECOSYSTEMS Tidal Salt Marshes Tidal Freshwater Marshes Mangrove Wetlands Tidal Estuarine Wetland 1 Definition and Formation of Estuaries u Estuary : partially

More information

Types of Wetlands. Tidal Systems

Types of Wetlands. Tidal Systems Types of Wetlands Tidal Systems 1 COASTAL WETLAND ECOSYSTEMS Tidal Salt Marshes Tidal Freshwater Marshes Mangrove Wetlands 2 Tidal Estuarine Wetland 3 Definition and Formation of Estuaries Estuary: : partially

More information

The Montauk Peninsula: Data and Preliminary Interpretations of the Ditch Plains Area Introduction

The Montauk Peninsula: Data and Preliminary Interpretations of the Ditch Plains Area Introduction The Montauk Peninsula: Data and Preliminary Interpretations of the Ditch Plains Area John A. Black GSI Patchogue, New York R.S. Welch Suffolk Community College Selden, New York Introduction Sirkin, (1982)

More information

Ridgeley Formation Pulpit Rock Weathering Rinds: Thickness of the Rind Compared to the Altitude and Location on the Formation

Ridgeley Formation Pulpit Rock Weathering Rinds: Thickness of the Rind Compared to the Altitude and Location on the Formation The JUNIATA JOURNAL of GEOLOGY, 1, 1-7 (2014) Original Article Ridgeley Formation Pulpit Rock Weathering Rinds: Thickness of the Rind Compared to the Altitude and Location on the Formation Jonathan Geyer

More information

1 Shoreline Landforms 2. 2 Emergent v. Submergent 2. 3 Wavecutting 3. 4 Planview 4. 5 Marine Terraces 5. 6 California 7. 7 Tombolos, Sea Stacks 8

1 Shoreline Landforms 2. 2 Emergent v. Submergent 2. 3 Wavecutting 3. 4 Planview 4. 5 Marine Terraces 5. 6 California 7. 7 Tombolos, Sea Stacks 8 Shorelines November 9, 2008 Contents 1 Shoreline Landforms 2 2 Emergent v. Submergent 2 3 Wavecutting 3 4 Planview 4 5 Marine Terraces 5 6 California 7 7 Tombolos, Sea Stacks 8 8 Active Processes 9 9 Emergence

More information

8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound

8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound 8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound Cockburn Sound is 20km south of the Perth-Fremantle area and has two features that are unique along Perth s metropolitan coast

More information

Feet. SAND; clayey, fine grained; shells are common; rounded quartz grains. SHELLS; muddy; almost no sand, shells and fragments common

Feet. SAND; clayey, fine grained; shells are common; rounded quartz grains. SHELLS; muddy; almost no sand, shells and fragments common SAND; clayey, fine grained; shells are common; rounded quartz grains SHELLS; muddy; almost no sand, shells and fragments common SAND; back to medium to fine; has a mottled appearance and looks burrowed;

More information

Coastal Oceanography. Coastal Oceanography. Coastal Waters

Coastal Oceanography. Coastal Oceanography. Coastal Waters Coastal Oceanography Coastal Oceanography 95% of ocean life is in coastal waters (320 km from shore) Estuaries and wetlands are among most productive ecosystems on Earth Major shipping routes, oil and

More information

Third Annual Monitoring Report Tidal Wetland Restoration 159 Long Neck Point Road, Darien, CT NAE

Third Annual Monitoring Report Tidal Wetland Restoration 159 Long Neck Point Road, Darien, CT NAE 1) Project Overview Third Annual Monitoring Report Tidal Wetland Restoration 159 Long Neck Point Road, Darien, CT NAE-2007-1130 December 15, 2014 This is the third year of a five year monitoring program

More information

Land subsidence due to groundwater withdrawal in Hanoi, Vietnam

Land subsidence due to groundwater withdrawal in Hanoi, Vietnam Land Subsidence (Proceedings of the Fifth International Symposium on Land Subsidence, The Hague, October 1995). 1AHS Publ. no. 234, 1995. 55 Land subsidence due to groundwater withdrawal in Hanoi, Vietnam

More information

The Geology of Two Lights State Park. Cape Elizabeth, Maine

The Geology of Two Lights State Park. Cape Elizabeth, Maine Maine Geologic Facts and Localities June, 2002 Cape Elizabeth, Maine 43 33 33.48 N, 70 12 13.32 W Text by Henry N. Berry IV and Robert G. Marvinney, Department of Agriculture, Conservation & Forestry 1

More information

Chapter 7 Case study. Sand dune coastal environment: Studland Bay

Chapter 7 Case study. Sand dune coastal environment: Studland Bay Sand dune coastal environment: Studland Bay Sand dunes are common features of low-lying stretches of coastline in the UK and elsewhere in the world. They form in places where there is a plentiful supply

More information

The Niagara Escarpment extends from western New York, through the GTA all the way up to Manitoulin Island and into Michigan and Wisconsin.

The Niagara Escarpment extends from western New York, through the GTA all the way up to Manitoulin Island and into Michigan and Wisconsin. is southern Ontario s most prominent topographic feature, extending more than 500 kilometres from western New York, through Niagara Falls and the western part of the Greater Toronto Area (GTA), and north

More information

Intertidal shellfish monitoring in the northern North Island region,

Intertidal shellfish monitoring in the northern North Island region, Intertidal shellfish monitoring in the northern North Island region, 2014 15 New Zealand Fisheries Assessment Report 2015/59 K. Berkenbusch P. Neubauer ISSN 1179-6480 (online) ISBN 978-1-77665-063-7 (online)

More information

INTER TIDAL DISTRIBUTION PATTERN OF FIVE COMMON GASTROPODS ALONG SAURASHTRA COAST, GUJARAT, INDIA

INTER TIDAL DISTRIBUTION PATTERN OF FIVE COMMON GASTROPODS ALONG SAURASHTRA COAST, GUJARAT, INDIA Electronic Journal of Environmental Sciences Vol. 8, 1-7 (2015) ISSN: 0973-9505 (Available online at www.tcrjournals.com) Original Article Indexed in: ProQuest database Abstract, USA ( ProQuest Science

More information

Section 2.1 Ocean Basins. - Has helped determine where ocean basins are located. - Tectonic plates move changing the position of the continents.

Section 2.1 Ocean Basins. - Has helped determine where ocean basins are located. - Tectonic plates move changing the position of the continents. Science 8 Unit 1: Water Systems on Earth Chapter 2: Oceans Control the Water Cycle Section 2.1 Ocean Basins Oceans are important because: 1. Primary water source for the water cycle 2. Control weather

More information

TASMANIAN SEAGRASS COMMUNITIES

TASMANIAN SEAGRASS COMMUNITIES TASMANIAN SEAGRASS COMMUNITIES by Christopher Grant Rees, B.Ed (}Ions.) Submitted in partial fulfilment of the requirement for the degree of Master of Environmental Studies (By Coursework) Centre for Environmental

More information

Aim and objectives Components of vulnerability National Coastal Vulnerability Assessment 2

Aim and objectives Components of vulnerability National Coastal Vulnerability Assessment 2 ASSESSING THE UTILITY OF GEOMORPHIC SENSITIVITY MAPPING ON THE ILLAWARRA COAST Pamela Abuodha, Christina Baker, Chris Sharples, Darren Skene and Colin Woodroffe Geoquest Research Centre, University of

More information

Continental Landscapes

Continental Landscapes Continental Landscapes Landscape influenced by tectonics, climate & differential weathering Most landforms developed within the last 2 million years System moves toward an equilibrium Continental Landscapes

More information

Short communication. Haloclasty on the bed of the Lake Gairdner salina, South Australia

Short communication. Haloclasty on the bed of the Lake Gairdner salina, South Australia Cadernos Lab. Xeolóxico de Laxe Coruña. 2008. Vol. 33, pp. 59-63 ISSN: 0213-4497 Short communication Haloclasty on the bed of the Lake Gairdner salina, South Australia TWIDALE, C. R. 1 and BOURNE, J. A.

More information

Geologic Mapping Regional Tournament Trial Event

Geologic Mapping Regional Tournament Trial Event Geologic Mapping Regional Tournament Trial Event A TEAM OF UP TO: 2 Team Name AVAILABLE TIME: 50 min Required Materials: Each team MUST have a protractor, ruler, non-programmable calculator, colored pencils,

More information

Create your own map for tidepooling, beach field trips, boating, camping, kayaking, fishing, and exploring the beaches in Southcentral Alaska.

Create your own map for tidepooling, beach field trips, boating, camping, kayaking, fishing, and exploring the beaches in Southcentral Alaska. Create your own map for tidepooling, beach field trips, boating, camping, kayaking, fishing, and exploring the beaches in Southcentral Alaska. Here s an opportunity to download and customize your own free

More information

A Geological Tour of Tumbledown Mountain, Maine

A Geological Tour of Tumbledown Mountain, Maine Maine Geologic Facts and Localities April, 1998 A Geological Tour of Tumbledown Mountain, Maine 44 45 3.21 N, 70 32 50.24 W Text by Robert G. Marvinney, Department of Agriculture, Conservation & Forestry

More information

The Geology of Sebago Lake State Park

The Geology of Sebago Lake State Park Maine Geologic Facts and Localities September, 2002 43 55 17.46 N, 70 34 13.07 W Text by Robert Johnston, Department of Agriculture, Conservation & Forestry 1 Map by Robert Johnston Introduction Sebago

More information

Chapter 9 Lecture Outline. Oceans: The Last Frontier

Chapter 9 Lecture Outline. Oceans: The Last Frontier Chapter 9 Lecture Outline Oceans: The Last Frontier The Vast World Ocean Earth is referred to as the blue planet 71% of Earth s surface is oceans and marginal seas Continents and islands comprise the remaining

More information

Unit 1: Water Systems on Earth Chapter 2

Unit 1: Water Systems on Earth Chapter 2 Unit 1: Water Systems on Earth Chapter 2 Create a mind map with the driving question, Why are Oceans Important? Remember: Why are oceans so important? Why are oceans so important? Primary water source

More information

Active Coastal Processes in the Lubec Embayment

Active Coastal Processes in the Lubec Embayment The Lubec Embayment Maine Geologic Facts and Localities August, 1998 Active Coastal Processes in the Lubec Embayment 44 49 50.51 N, 66 59 34.16 W Text by Joseph T. Kelley, Department of Agriculture, Conservation

More information