Beach Nourishment Alternatives for Mitigating Erosion of Ancient Coastal Sites on the Mediterranean Coast of Israel

Total Page:16

File Type:pdf, Size:1020Kb

Beach Nourishment Alternatives for Mitigating Erosion of Ancient Coastal Sites on the Mediterranean Coast of Israel Journal of Marine Science and Engineering Article Beach Nourishment Alternatives for Mitigating Erosion of Ancient Coastal Sites on the Mediterranean Coast of Israel Menashe Bitan 1, Ehud Galili 1,2, Ehud Spanier 1,3 and Dov Zviely 4,* 1 Department of Maritime Civilizations, The Leon H. Charney School for Marine Sciences, University of Haifa, 199 Aba-Khoushi Avenue, Mount Carmel, Haifa 3498838, Israel; [email protected] (M.B.); [email protected] (E.G.); [email protected] (E.S.) 2 Zinman Institute of Archaeology, University of Haifa, 199 Aba-Khoushi Avenue, Mount Carmel, Haifa 3498838, Israel 3 The Leon Recanati Institute for Maritime Studies, The Leon H. Charney School for Marine Sciences, University of Haifa, 199 Aba-Khoushi Avenue, Mount Carmel, Haifa 3498838, Israel 4 Faculty of Marine Sciences, Ruppin Academic Center, Emek-Hefer 40250, Israel * Correspondence: [email protected]; Tel.: +972-9-830-4149 Received: 26 June 2020; Accepted: 10 July 2020; Published: 12 July 2020 Abstract: Since 2011, beach nourishment has become the preferred solution for mitigating coastal erosion along the Mediterranean coast of Israel, as it is considered “soft” and environmentally friendly. However, using fine sand for nourishment in Israel without supporting measures is problematic due to the high wave energy and strong longshore currents in the littoral zone that tend to drift the sand away. This would require ongoing, multiyear, costly, and never-ending maintenance. In the present study, we analyzed sand and pebble alternatives for nourishment of the eroded beach in front of Tel Ashkelon, an important coastal archaeological site in southern Israel that suffers from severe erosion. Based on Pranzini et al. (2018), we analyzed the alternatives, evaluated their cost and efficiency, and assessed their potential environmental impacts. The study concluded that for protecting the southern part of Tel Ashkelon beach, pebble nourishment is the optimal solution, mainly regarding durability and cost. Using this material for nourishment will better absorb the storm wave impact and protect the foot of the archaeological Tel from erosion, and require lower maintenance cost than using finer sand nourishment. Keywords: coastal processes; dredging; nourishment durability; unit sand volume; pebbles; Levant; Tel Ashkelon 1. Introduction The Mediterranean Sea is rich in unique cultural assets and is considered to be the cradle of many civilizations, religions, and cultures [1,2]. Ancient empires and cultures have left a wealth of remains, including coastal settlements, harbors, and anchorages. Some of the most important ancient sites, which represent the mutual relation between man and the sea, are located on the Mediterranean coast of Israel [3–5]. During the 20th century, Israeli ancient coastal sites such as (from south to north) Tel Ashkelon, Yavneh-Yam, Apollonia, Caesarea, Dor, Atlit, and Akko (Acre) (Figure1: top inset), have been severely eroded, mainly due to modern marine construction, as well as sea level rise, and storm waves [1,4,6,7]. If these processes continue, a significant portion of the marine heritage of humanity will disappear, and archaeological and touristic assets of great cultural, scientific and economic value will be lost [1,4]. This coastal erosion may also affect the unique intertidal ecosystems at these sites [8]. J. Mar. Sci. Eng. 2020, 8, 509; doi:10.3390/jmse8070509 www.mdpi.com/journal/jmse J. Mar. Sci. Eng. 2020, 8, x FOR PEER REVIEW 2 of 15 touristicJ. Mar. Sci. assets Eng. 2020 of, 8great, 509 cultural, scientific and economic value will be lost [1,4]. This coastal erosion2 of 15 may also affect the unique intertidal ecosystems at these sites [8]. Figure 1. AshkelonAshkelon coast, coast, the main mari marinene constructions and Tel AshkelonAshkelon site (Photo: Google Earth image,image, 2828 JanuaryJanuary 2016) 2016) (EAPC—Eilat-Ashkelon (EAPC—Eilat-Ashkelon Pipeline Pipeline Company); Company); The The Mediterranean Mediterranean coast coast of Israel of Israeland its and main its ancientmain ancient coastal coastal sites (top sites left (top inset); left The inset); Nile The littoral Nile cell littoral longshore cell longshore sand transport sand transport direction direction(black arrows), (black fromarrows), the Nilefrom Delta the Nile to Haifa Delta Bay to Haifa (bottom Bay right (bottom inset). right inset). One of the most important archaeological sites sites on the Israeli coast is Tel Ashkelon (ancient Ashkelon) [9–11], [9–11], situated within the Ashkelon Nati Nationalonal Park, adjacent to to the southern part of the modern city of Ashkelon (Figures 11 andand2 2).). TheThe mostmost prominentprominent ruins ruins seen seen today today in in Tel Tel Ashkelon Ashkelon are are the Crusader fortificationsfortifications (638-1187 (638-1187 CE) CE) [12 [12–14].–14]. These These remains remains include include several several sections sections of the of oldthe cityold citywall wall and and a short a short part part (40 m(40 long) m long) of its of seaside its seaside wall wall (i.e., (i.e., the Columnsthe Columns wall) wall) (Figure (Figure3). The 3). latterThe latter was wasreinforced reinforced by the by Crusaders, the Crusaders, who reused who granite reused columns granite taken columns from taken Roman from/Hellenistic Roman/Hellenistic monumental monumentalstructures [15 structures]. [15]. J. Mar. Sci. Eng. 2020, 8, 509 3 of 15 J.J. Mar.Mar. Sci.Sci. Eng.Eng. 2020,, 8,, xx FORFOR PEERPEER REVIEWREVIEW 33 ofof 1515 Figure 2.2. TelTel Ashkelon Ashkelon and and its its coast, coast, showing showing the erodedthe eroded beach beach (0–15 (0–15 m wide) m wide) (between (between the red the arrows) red arrows)at the vicinity at the ofvicinity the Columns of the Co wall,lumnslumns and wall,wall, the and widerand thethe (30–50 widerwider m) (30–50(30–50 sandy m)m) beach sandysandy (between beachbeach (between(between the yellow thethearrows) yellowyellow arrows)at the vicinity at the ofvicinity the bathing of the beachbathing (Photo: beach A(Pho rotatedto: A Googlerotated EarthGoogle image, Earth 28 image, January 28 January 2016). 2016). Figure 3. View to northeast of the eroded beach in southern Tel Ashkelon, at the vicinity of the Figure 3.3. ViewView to to northeast northeast of of the the eroded eroded beach beach in southern in southern Tel Ashkelon, Tel Ashkelon, at the vicinity at the ofvicinity the Columns of the wallColumns (photographed wall (photographed by Dov Zviely, by Dov 19 Zviely, December 19 December 2019). 2019). Because ofof thethe importanceimportance of of the the archaeological archaeological remains remains along along the the coast coast of Telof Tel Ashkelon, Ashkelon, it is it our is ourduty duty to preserve to preserve them them for the for sake the ofsake future of future generations. generations. Several Several plans haveplans been have proposed been proposed in the last in 15the years last by15 governmentalyears by governmental agencies; however,agencies; only however, one project only aimedone project at protecting aimed theat protecting Columns wall the Columnshas been completedwall has been so far. completed The Columns so far.far.wall TheThe wasColumnsColumns protected wallwall bywaswas building protectedprotected a ‘sacrificial’ byby buildingbuilding layer aa ‘sacrificial’‘sacrificial’ of stones (3layer m highof stones and (3 1 m m thick)high and on its1 m seaward thick) on side. its se Theaward project side. was The carried project outwas by carried the Israel out by Antiquities the Israel AuthorityAntiquities in Authority 2005. in 2005. Beach nourishmentnourishment isis one one of of the the commonest commonest ‘soft ‘soft solutions’ solutions’ for for coastal coastal erosion erosion [16– [16–21],21], and and it was it wasfound found more more appropriate appropriate from from environmental environmental and economicaland economical perspectives, perspectives, than than ‘hard ‘hard solutions’, solutions’, such suchas seawalls, as seawalls, revetments, revetments, detached detached breakwaters, breakwaters, and groinsand groins [22]. Studies[22]. Studies have have revealed revealed that athat clear a cleardefinition definition of the aimsof the of aims beach of nourishment beach nourishment and a well-based and a well-based knowledge knowledge of the local of physical the local conditions physical (e.g.,conditions coastal (e.g., morphology, coastal morphology, native sediment native grain sedi size,ment wave grain regime) size, are wave crucial regime) for a successfulare crucial coastal for a protectionsuccessful projectcoastal[ 21protection]. Furthermore, project to [21]. achieve Furthermore, a successful to nourishment,achieve a successful a cost-e ffnourishment,ectiveness approach a cost- effectivenessis needed, together approach with is an needed, analysis oftogether alternative with solutions, an analysis effective of alternative planning andsolutions, monitoring, effective and planningusing compatible and monitoring, sediment and for using nourishment compatib [21le,23 sediment,24]. for nourishment [21,23,24]. The presentpresent studystudy analyzesanalyzes sandsand and and pebble pebble alternatives alternatives for for nourishment nourishment of of the the eroded eroded beach beach in inthe the vicinity vicinity of theof the Columns Columns wall wall in Tel in Ashkelon.Tel Ashkel Theon. The study study evaluates evaluates the costthe andcost eandfficiency efficiency of each of each alternative, examines their potential environmental impacts, and suggests
Recommended publications
  • Coastal Erosion - Orrin H
    COASTAL ZONES AND ESTUARIES – Coastal Erosion - Orrin H. Pilkey, William J. Neal, David M. Bush COASTAL EROSION Orrin H. Pilkey Program for the Study of Developed Shorelines, Division of Earth and Ocean Sciences, Duke University, Durham, NC, U.S.A. William J. Neal Department of Geology, Grand Valley State University, Allendale, MI, USA. David M. Bush Department of Geosciences, State University of West Georgia, Carrollton, GA, USA. Keywords: erosion, shoreline retreat, sea level rise, barrier islands, beach, coastal management, shoreline armoring, seawalls, sand supply Contents 1. Introduction 2. Causes of Erosion 2.1. Sea Level Rise 2.2. Sand Supply 2.3. Shoreline Engineering 2.4. Wave Energy and Storm Frequency 3. "Special" Cases 4. Solutions to Coastal Erosion 5. The Future Glossary Bibliography Biographical Sketches Summary Almost all of the world’s shorelines are retreating in a landward direction—a process called shoreline erosion. Sea level rise and the reduction of sand supply to the shoreline by damming of rivers, armoring of shorelines and the dredging of navigation channels are among the major causes of shoreline retreat. As sea levels continue to rise, sometimesUNESCO enhanced by subsidence caused – byEOLSS oil and water extraction, global erosion rates should increase in coming decades. Three response alternatives are available to "solve" the erosionSAMPLE problem. These are cons tructionCHAPTERS of seawalls and other engineering structures, beach nourishment and relocation or abandonment of buildings. No matter what path is chosen, response to the erosion problem is costly. 1. Introduction Coastal erosion is a major problem for developed shorelines everywhere in the world. Such erosion is regarded as a coastal hazard and is a common focus of local and national coastal management.
    [Show full text]
  • Coastal Flood Defences - Groynes
    Coastal Flood Defences - Groynes Coastal flood defences are key to protecting our coasts against flooding, which is when normally dry, low lying flat land is inundated by sea water. Hard engineering methods are forms of coastal flood defences which mitigate the risk of flooding and coastal erosion and the consequential effects. Hard Engineering Hard engineering methods are often used as a temporary measure to protect against coastal flooding as they are costly and only last for a relatively short amount of time before they require maintenance. However, they are very effective at protecting the coastline in the short-term as they are immediately effective as opposed to some longer term soft engineering methods. But they are often intrusive and can cause issues elsewhere at other areas along the coastline. Groynes are low lying wood or concrete structures which are situated out to sea from the shore. They are designed to trap sediment, dissipate wave energy and restrict the transfer of sediment away from the beach through long shore drift. Longshore drift is caused when prevailing winds blow waves across the shore at an angle which carries sediment along the beach.Groynes prevent this process and therefore, slow the process of erosion at the shore. They can also be permeable or impermeable, permeable groynes allow some sediment to pass through and some longshore drift to take place. However, impermeable groynes are solid and prevent the transfer of any sediment. Advantages and Disadvantages +Groynes are easy to construct. +They have long term durability and are low maintenance. +They reduce the need for the beach to be maintained through beach nourishment and the recycling of sand.
    [Show full text]
  • Coastal Processes and Causes of Shoreline Erosion and Accretion Causes of Shoreline Erosion and Accretion
    Coastal Processes and Causes of Shoreline Erosion and Accretion and Accretion Erosion Causes of Shoreline Heather Weitzner, Great Lakes Coastal Processes and Hazards Specialist Photo by Brittney Rogers, New York Sea Grant York Photo by Brittney Rogers, New New York Sea Grant Waves breaking on the eastern Lake Ontario shore. Wayne County Cooperative Extension A shoreline is a dynamic environment that evolves under the effects of both natural 1581 Route 88 North and human influences. Many areas along New York’s shorelines are naturally subject Newark, NY 14513-9739 315.331.8415 to erosion. Although human actions can impact the erosion process, natural coastal processes, such as wind, waves or ice movement are constantly eroding and/or building www.nyseagrant.org up the shoreline. This constant change may seem alarming, but erosion and accretion (build up of sediment) are natural phenomena experienced by the shoreline in a sort of give and take relationship. This relationship is of particular interest due to its impact on human uses and development of the shore. This fact sheet aims to introduce these processes and causes of erosion and accretion that affect New York’s shorelines. Waves New York’s Sea Grant Extension Program Wind-driven waves are a primary source of coastal erosion along the Great provides Equal Program and Lakes shorelines. Factors affecting wave height, period and length include: Equal Employment Opportunities in 1. Fetch: the distance the wind blows over open water association with Cornell Cooperative 2. Length of time the wind blows Extension, U.S. Department 3. Speed of the wind of Agriculture and 4.
    [Show full text]
  • The Mediterranean Coast of Israel Is a New City,Now Under
    University of Rhode Island DigitalCommons@URI Theses and Major Papers Marine Affairs 12-1973 The editM erranean Coast of Israel: A Planner's Approach Sophia Professorsky University of Rhode Island Follow this and additional works at: http://digitalcommons.uri.edu/ma_etds Part of the Natural Resources Management and Policy Commons, and the Oceanography and Atmospheric Sciences and Meteorology Commons Recommended Citation Professorsky, Sophia, "The eM diterranean Coast of Israel: A Planner's Approach" (1973). Theses and Major Papers. Paper 146. This Major Paper is brought to you for free and open access by the Marine Affairs at DigitalCommons@URI. It has been accepted for inclusion in Theses and Major Papers by an authorized administrator of DigitalCommons@URI. For more information, please contact [email protected]. l~ .' t. ,." ,: .. , ~'!lB~'MEDI'1'ERRANEAN-GQAsT ~F.~"IsMt~·;.·(Al!~.oS:-A~PROACH ::".~~========= =~.~~=~~~==b======~~==~====~==.=~=====~ " ,. ••'. '. ,_ . .. ... ..p.... "".. ,j,] , . .;~ ; , ....: ./ :' ",., , " ",' '. 'a ". .... " ' ....:. ' ' .."~".,. :.' , v : ".'. , ~ . :)(A;R:t.::·AF'~~RS'· B~NMi'»APER. '..":. " i . .: '.'-. .: " ~ . : '. ". ..." '-" .~" ~-,.,. .... .., ''-~' ' -.... , . ", ~,~~~~"ed .' bYr. SOph1a,Ji~ofes.orsJcy .. " • "..' - 01 .,.-~ ~ ".··,::.,,;$~ld~~:' ·to,,:" f;~f.... ;)J~:Uexa~d.r . -". , , . ., .."• '! , :.. '> ...; • I ~:'::':":" '. ~ ... : .....1. ' ..~fn··tr8Jti~:·'btt·,~e~Mar1ne.~a1~S·~r~~. ", .:' ~ ~ ": ",~', "-". ~_"." ,' ~~. ;.,·;·X;'::/: u-=" .. _ " -. • ',. ,~,At:·;t.he ,un:lvers:U:~; tif Rh~:<:rs1..J\d. ~ "~.; ~' ~.. ~,- -~ !:).~ ~~~ ~,: ~:, .~ ~ ~< .~ . " . -, -. ... ... ... ... , •• : ·~·J;t.1l9ston.l~~;&:I( .. t)eceiDber; 1~73.• ". .:. ' -.. /~ NOTES, ===== 1. Prior to readinq this paper, please study the map of the country (located in the back-eover pocket), in order to get acquain:t.ed with names and locations of sites mentioned here thereafter. 2.- No ~eqaJ. aspects were introduced in this essay since r - _.-~ 1 lack the professional background for feedinq in tbe information.
    [Show full text]
  • Management of Coastal Erosion by Creating Large-Scale and Small-Scale Sediment Cells
    COASTAL EROSION CONTROL BASED ON THE CONCEPT OF SEDIMENT CELLS by L. C. van Rijn, www.leovanrijn-sediment.com, March 2013 1. Introduction Nearly all coastal states have to deal with the problem of coastal erosion. Coastal erosion and accretion has always existed and these processes have contributed to the shaping of the present coastlines. However, coastal erosion now is largely intensified due to human activities. Presently, the total coastal area (including houses and buildings) lost in Europe due to marine erosion is estimated to be about 15 km2 per year. The annual cost of mitigation measures is estimated to be about 3 billion euros per year (EUROSION Study, European Commission, 2004), which is not acceptable. Although engineering projects are aimed at solving the erosion problems, it has long been known that these projects can also contribute to creating problems at other nearby locations (side effects). Dramatic examples of side effects are presented by Douglas et al. (The amount of sand removed from America’s beaches by engineering works, Coastal Sediments, 2003), who state that about 1 billion m3 (109 m3) of sand are removed from the beaches of America by engineering works during the past century. The EUROSION study (2004) recommends to deal with coastal erosion by restoring the overall sediment balance on the scale of coastal cells, which are defined as coastal compartments containing the complete cycle of erosion, deposition, sediment sources and sinks and the transport paths involved. Each cell should have sufficient sediment reservoirs (sources of sediment) in the form of buffer zones between the land and the sea and sediment stocks in the nearshore and offshore coastal zones to compensate by natural or artificial processes (nourishment) for sea level rise effects and human-induced erosional effects leading to an overall favourable sediment status.
    [Show full text]
  • Emergency in Israel
    Emergency in Israel Emergency Update on Jewish Agency Programming May 16, 2021 The recent violent events that have erupted across the country have left us all surprised and stunned: clashes with Palestinians in Jerusalem and on the Temple Mount; the deteriorating security tensions and the massive barrage of missiles from Gaza on southern and central Israel; and the outbreak of unprecedented violence, destruction, and lynching in mixed cities and Arab communities. To say that the situation is particularly challenging is an understatement. We must all deal with the consequences of the current tensions. Many of us are protecting family, coworkers, or people under our charge while missiles fall on our heads night and day, forcing us to seek shelter. We have all witnessed the unbearable sights of rioting, beating, and arson by Arab and Jewish extremists in Lod, Ramla, Acre, Kfar Qassem, Bat Yam, Holon, and other places. As an organization that has experienced hard times of war and destruction, as well as periods of prosperity and peace, it is our duty to rise up and make a clear statement: we will support and assist populations hit by missile fire as we did in the past, after the Second Lebanon War and after Operations Cast Lead and Protective Edge. Together with our partners, we will mobilize to heal and support the communities and populations affected by the fighting. Our Fund for Victims of Terror is already providing assistance to bereaved families. When the situation allows it, we will provide more extensive assistance to localities and communities that have suffered damage and casualties.
    [Show full text]
  • Timeline of Shīʿī History in Palestine
    Timeline of Shīʿī History in Palestine Umayyads – Early second/eighth century: People from Palestine send a convoy to the Imām Jaʿfar al-Ṣādiq. ʿAbbāsids – Second half of the third/ninth century: The geographer al-Yaʿqūbī mentions the settlement of the Shīʿī ʿĀmila tribe in the Jund Filasṭīn. – 271/884: Muḥammad b. Ḥamza, a descendant of al-ʿAbbās b. ʿAlī, is murdered in Tiberias by Ṭughj b. Juff the Ikhshīdid. – 289–90/902–03: The Ismāʿīlī mahdī of Salamiyya, ʿAbdallāh al-Mahdī, hides in Ramla. – First half of the fourth/tenth century: The Persian Shīʿī poet Kushājim sojourns in Ramla. Fāṭimids – Second half of the fourth/tenth century: The geographer Muḥammad al-Maqdisī complains that all Tiberias, half of Nablus, and Qadas are Shīʿīs. – 360–67/970–77: The Qarmaṭī invasion of Palestine is centered in Ramla. – 363–64/973–74: Authorities imposed Shīʿī customs in Palestine, two Sunnīs from Ramla and Jerusalem who opposed it were detained and tortured. – 386/996: Shīʿī messianic rebellion of Abū l-Futūḥ Ḥasan b. Jaʿfar, the amīr of Mecca in Ramla. – First half of the fifth/eleventh century: – Shīʿī genealogist Najm al-Dīn al-ʿUmarī travels through Ramla, and mentions several Ṭālibiyyūn (descendants of the Imāms) in Jerusalem, Tiberias, and Ramla. – The Sunnī Ibn Ḥazm al-Andalusī complains that all of Urdunn (that is, Galilee), mainly Tiberias, is controlled by the Nuṣayrīs (now ʿAlawīs). – Druzes/Ḥākimī spread propaganda in Galilee (al-Buqayʿa) and Ḥamza’s oppo- nents are mentioned in Acre. © Koninklijke Brill NV, Leiden, 2020 | doi:10.1163/9789004421028_015 Yaron Friedman - 9789004421028 Downloaded from Brill.com09/28/2021 04:13:15AM via free access Timeline 203 – Mid-fifth/eleventh century: The traveler Nāṣir Khusraw mentions Shīʿīs in Tiberias and Fāṭimid investment and construction projects in Palestine.
    [Show full text]
  • Linktm Gabions and Mattresses Design Booklet
    LinkTM Gabions and Mattresses Design Booklet www.globalsynthetics.com.au Australian Company - Global Expertise Contents 1. Introduction to Link Gabions and Mattresses ................................................... 1 1.1 Brief history ...............................................................................................................................1 1.2 Applications ..............................................................................................................................1 1.3 Features of woven mesh Link Gabion and Mattress structures ...............................................2 1.4 Product characteristics of Link Gabions and Mattresses .........................................................2 2. Link Gabions and Mattresses .............................................................................. 4 2.1 Types of Link Gabions and Mattresses .....................................................................................4 2.2 General specification for Link Gabions, Link Mattresses and Link netting...............................4 2.3 Standard sizes of Link Gabions, Mattresses and Netting ........................................................6 2.4 Durability of Link Gabions, Link Mattresses and Link Netting ..................................................7 2.5 Geotextile filter specification ....................................................................................................7 2.6 Rock infill specification .............................................................................................................8
    [Show full text]
  • INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The
    INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The Intertidal Zone is the narrow belt along the shoreline lying between the lowest and highest tide marks. The intertidal or littoral zone is subdivided broadly into four vertical zones based on the amount of time the zone is submerged. From highest to lowest, they are Supratidal or Spray Zone Upper Intertidal submergence time Middle Intertidal Littoral Zone influenced by tides Lower Intertidal Subtidal Sublittoral Zone permanently submerged The intertidal zone may also be subdivided on the basis of the vertical distribution of the species that dominate a particular zone. However, zone divisions should, in most cases, be regarded as approximate! No single system of subdivision gives perfectly consistent results everywhere. Please refer to the intertidal zonation scheme given in the attached table (last page). Zonal Distribution of organisms is controlled by PHYSICAL factors (which set the UPPER limit of each zone): 1) tidal range 2) wave exposure or the degree of sheltering from surf 3) type of substrate, e.g., sand, cobble, rock 4) relative time exposed to air (controls overheating, desiccation, and salinity changes). BIOLOGICAL factors (which set the LOWER limit of each zone): 1) predation 2) competition for space 3) adaptation to biological or physical factors of the environment Species dominance patterns change abruptly in response to physical and/or biological factors. For example, tide pools provide permanently submerged areas in higher tidal zones; overhangs provide shaded areas of lower temperature; protected crevices provide permanently moist areas. Such subhabitats within a zone can contain quite different organisms from those typical for the zone.
    [Show full text]
  • 2624 Israel 0I-07-3C
    ANCIENT ISRAEL REVEALED June 16 - July 3, 2007 Saturday, June 16: CHICAGO/TEL AVIV Depart Chicago in the evening. Sunday, June 17: JERUSALEM: David Citadel Hotel We arrive into Ben Gurion Airport and drive up to Jerusalem to Dear Members and Friends of the Oriental Institute: rest before our orientation lecture and dinner. (D) The Oriental Institute is pleased to present a comprehensive Monday, June 18: JERUSALEM: David Citadel Hotel tour of Israel. Uniquely situated at the crossroads of cultures, Touring begins on the Mt. of Olives and Mt. Scopus. Viewing Israel is among the most historically rich areas in the world. The Jerusalem from this perspective gives us an understanding of the Oriental Institute has had an archaeological presence there historical ramifications of its location. We enter the Old City at the Citadel built by Herod, and begin our historical overview from its since the early 1900s, when founder James Henry Breasted sent walls. Today’s Old City touring will focus on the First Temple an expedition to excavate at the site of Megiddo. The dig period including Hezekiah’s fortifications and the City of David, covered a span in time from 5000 to 600 BC. Each layer was where excavations have exposed the city and shaft leading to the carefully uncovered to reveal successive cultures that city’s water supply in the Kidron Valley. We will examine dominated the city. In 2005, the Haas and Schwartz Megiddo Hezekiah’s Tunnel, built through the rock to divert the water into Gallery opened at the Oriental Institute Museum, featuring an inner city reservoir, the Gihon Spring and pool of Siloam.
    [Show full text]
  • Beach Nourishment: Massdep's Guide to Best Management Practices for Projects in Massachusetts
    BBEACHEACH NNOURISHMEOURISHMENNTT MassDEP’sMassDEP’s GuideGuide toto BestBest ManagementManagement PracticesPractices forfor ProjectsProjects inin MassachusettsMassachusetts March 2007 acknowledgements LEAD AUTHORS: Rebecca Haney (Coastal Zone Management), Liz Kouloheras, (MassDEP), Vin Malkoski (Mass. Division of Marine Fisheries), Jim Mahala (MassDEP) and Yvonne Unger (MassDEP) CONTRIBUTORS: From MassDEP: Fred Civian, Jen D’Urso, Glenn Haas, Lealdon Langley, Hilary Schwarzenbach and Jim Sprague. From Coastal Zone Management: Bob Boeri, Mark Borrelli, David Janik, Julia Knisel and Wendolyn Quigley. Engineering consultants from Applied Coastal Research and Engineering Inc. also reviewed the document for technical accuracy. Lead Editor: David Noonan (MassDEP) Design and Layout: Sandra Rabb (MassDEP) Photography: Sandra Rabb (MassDEP) unless otherwise noted. Massachusetts Massachusetts Office Department of of Coastal Zone Environmental Protection Management 1 Winter Street 251 Causeway Street Boston, MA Boston, MA table of contents I. Glossary of Terms 1 II. Summary 3 II. Overview 6 • Purpose 6 • Beach Nourishment 6 • Specifications and Best Management Practices 7 • Permit Requirements and Timelines 8 III. Technical Attachments A. Beach Stability Determination 13 B. Receiving Beach Characterization 17 C. Source Material Characterization 21 D. Sample Problem: Beach and Borrow Site Sediment Analysis to Determine Stability of Nourishment Material for Shore Protection 22 E. Generic Beach Monitoring Plan 27 F. Sample Easement 29 G. References 31 GLOSSARY Accretion - the gradual addition of land by deposition of water-borne sediment. Beach Fill – also called “artificial nourishment”, “beach nourishment”, “replenishment”, and “restoration,” comprises the placement of sediment within the nearshore sediment transport system (see littoral zone). (paraphrased from Dean, 2002) Beach Profile – the cross-sectional shape of a beach plotted perpendicular to the shoreline.
    [Show full text]
  • Appendix 1 : Marine Habitat Types Definitions. Update Of
    Appendix 1 Marine Habitat types definitions. Update of “Interpretation Manual of European Union Habitats” COASTAL AND HALOPHYTIC HABITATS Open sea and tidal areas 1110 Sandbanks which are slightly covered by sea water all the time PAL.CLASS.: 11.125, 11.22, 11.31 1. Definition: Sandbanks are elevated, elongated, rounded or irregular topographic features, permanently submerged and predominantly surrounded by deeper water. They consist mainly of sandy sediments, but larger grain sizes, including boulders and cobbles, or smaller grain sizes including mud may also be present on a sandbank. Banks where sandy sediments occur in a layer over hard substrata are classed as sandbanks if the associated biota are dependent on the sand rather than on the underlying hard substrata. “Slightly covered by sea water all the time” means that above a sandbank the water depth is seldom more than 20 m below chart datum. Sandbanks can, however, extend beneath 20 m below chart datum. It can, therefore, be appropriate to include in designations such areas where they are part of the feature and host its biological assemblages. 2. Characteristic animal and plant species 2.1. Vegetation: North Atlantic including North Sea: Zostera sp., free living species of the Corallinaceae family. On many sandbanks macrophytes do not occur. Central Atlantic Islands (Macaronesian Islands): Cymodocea nodosa and Zostera noltii. On many sandbanks free living species of Corallinaceae are conspicuous elements of biotic assemblages, with relevant role as feeding and nursery grounds for invertebrates and fish. On many sandbanks macrophytes do not occur. Baltic Sea: Zostera sp., Potamogeton spp., Ruppia spp., Tolypella nidifica, Zannichellia spp., carophytes.
    [Show full text]