志錄實體軸 / 吐露港 / 地方

吐露港 · 原文未繫年

Tolo Harbour · Undated in the source

呢一頁係「吐露港」呢條軸嘅原文未繫年,共 76 條條目(公元 undated 至 undated)。 逐條附第一官方來源、原書頁碼同「引用呢條」。

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《香港志·自然》自然資源與生態 Hong Kong Chronicles, Nature: Natural Resources and Ecology

中文腳註香港地方志中心,《香港志·自然》自然資源與生態(查閱日期 2026-10-18),頁 〈頁碼〉,/chronicle/archive/undated#〈條目編號〉。

APAHong Kong Chronicles Institute. Hong Kong Chronicles, Nature: Natural Resources and Ecology (p. 〈頁碼〉). Accessed 2026-10-18. /chronicle/archive/undated#〈條目編號〉

《香港志·自然》建置與地區概況(人口) Hong Kong Chronicles, Nature: Territory, Geography and Population

中文腳註香港地方志中心,《香港志·自然》建置與地區概況(人口)(查閱日期 2026-10-18),頁 〈頁碼〉,/chronicle/archive/undated/6#〈條目編號〉。

APAHong Kong Chronicles Institute. Hong Kong Chronicles, Nature: Territory, Geography and Population (p. 〈頁碼〉). Accessed 2026-10-18. /chronicle/archive/undated/6#〈條目編號〉

《香港志·自然》環境保護與生態保育 Hong Kong Chronicles, Nature: Environmental Protection and Conservation

中文腳註香港地方志中心,《香港志·自然》環境保護與生態保育(查閱日期 2026-10-18),頁 〈頁碼〉,/chronicle/archive/undated/7#〈條目編號〉。

APAHong Kong Chronicles Institute. Hong Kong Chronicles, Nature: Environmental Protection and Conservation (p. 〈頁碼〉). Accessed 2026-10-18. /chronicle/archive/undated/7#〈條目編號〉

《香港志·自然》自然環境 Hong Kong Chronicles, Nature: Natural Environment

中文腳註香港地方志中心,《香港志·自然》自然環境(查閱日期 2026-10-18),頁 〈頁碼〉,/chronicle/archive/undated/9#〈條目編號〉。

APAHong Kong Chronicles Institute. Hong Kong Chronicles, Nature: Natural Environment (p. 〈頁碼〉). Accessed 2026-10-18. /chronicle/archive/undated/9#〈條目編號〉

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汀角攀樹蟹亦見於吐露港西徑及西貢土瓜坪的紅樹林,現時僅香港有記錄。

The Ting Kok tree-climbing crab is also found in the mangroves of Sai Keng in Tolo Harbour and To Kwu Pai in Sai Kung, and is currently recorded only in Hong Kong.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.413

吐露港海星灣與企嶺下海泥灘曾錄得25平方米範圍內逾700隻和尚蟹聚集覓食。

More than 700 soldier crabs were recorded gathering to feed within a 25-square-metre area at Starfish Bay in Tolo Harbour and the Kei Ling Ha sea mudflat.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.415

由南漢時期起,直至明代,吐露港一直是各朝政府進行採集珍珠的重要地點。

From the Southern Han period until the Ming dynasty, Tolo Harbour was an important site for pearl gathering by successive governments.

來源 《香港志·自然》建置與地區概況(人口)(香港地方志中心) · p.143

大埔吐露港水體交換平均需時28天,初夏易出現紅潮。

The water in Tolo Harbour in Tai Po takes an average of 28 days to exchange, and red tides tend to occur in early summer.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.274

東部水域由大鵬灣、牛尾海、吐露港與赤門合共四個水質管制區組成。

The eastern waters consist of four water quality control zones: Mirs Bay, Port Shelter, Tolo Harbour and Tolo Channel.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.376

吐露港的水質指標達標率通常介於50%至80%。

The compliance rate with water quality objectives in Tolo Harbour is usually between 50% and 80%.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.376

吐露港腹地包括沙田與大埔等新市鎮,並有舊村落及禽畜農場未接駁污水收集系統。

The hinterland of Tolo Harbour includes new towns such as Sha Tin and Tai Po, as well as old villages and livestock farms not connected to the sewerage system.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.376

吐露港集水區每年經地下水排入海洋的水量,估計達0.77億立方米左右。

The annual volume of water discharged to the sea via groundwater from the Tolo Harbour catchment is estimated at about 77 million cubic metres.

來源 《香港志·自然》自然環境(香港地方志中心) · p.434

吐露港集水區內河流每年注入海洋的徑流總量達0.94億立方米。

Rivers within the Tolo Harbour catchment discharge a total of 94 million cubic metres of runoff into the sea each year.

來源 《香港志·自然》自然環境(香港地方志中心) · p.434

吐露港溶解氧達標率長期偏低,部分年度達標率為零。

The dissolved oxygen compliance rate in Tolo Harbour has long been low, with a rate of zero in some years.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.376

吐露港水質近30年來獲得穩定改善。

The water quality of Tolo Harbour has improved steadily over the past 30 years.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.376

吐露港為半封閉淺水水體,出口狹窄,與大鵬灣的水交換率偏低。

Tolo Harbour is a semi-enclosed shallow water body with a narrow outlet and a low water exchange rate with Mirs Bay.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.376

吐露港一帶水質明顯較大鵬灣及牛尾海為差,而大鵬灣與牛尾海兩處則基本維持於較佳水平。

Water quality around Tolo Harbour is noticeably worse than that of Mirs Bay and Port Shelter, while Mirs Bay and Port Shelter basically remain at a better level.

來源 《香港志·自然》自然環境(香港地方志中心) · p.507

夏季吐露港常出現水溫與鹽度分層,阻礙水體混合,容易造成海底缺氧。

In summer, Tolo Harbour often experiences temperature and salinity stratification, which hinders water mixing and easily causes hypoxia on the seabed.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.376

香港東部水域包含大鵬灣、牛尾海及吐露港及赤門三個水質管制區。

The eastern waters of Hong Kong include three water quality control zones: Mirs Bay, Port Shelter, and Tolo Harbour and Channel.

來源 《香港志·自然》自然環境(香港地方志中心) · p.505

在吐露港、大鵬灣與南區水域,浮游植物總密度處於較高水平;932次紅潮事件裏,大約有七成是發生於這三個地點。

In Tolo Harbour, Mirs Bay and the waters of the Southern District, total phytoplankton density is relatively high; of 932 red tide incidents, about 70% occurred at these three locations.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.381

在吐露港與大鵬灣內灣所收集的翡翠貽貝,其完整性表現較佳;至於馬灣、索罟灣及尖沙咀的樣本,完整性則相對偏低。

Green-lipped mussels collected in Tolo Harbour and the inner Tolo Channel of Mirs Bay showed better integrity, while samples from Ma Wan, Sok Kwu Wan and Tsim Sha Tsui showed relatively low integrity.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.387

踏入二十世紀後,大埔與吐露港區域受風暴潮衝擊尤為顯著。

After entering the twentieth century, the Tai Po and Tolo Harbour areas were particularly significantly affected by storm surges.

來源 《香港志·自然》自然環境(香港地方志中心) · p.591

被岬角遮蔽的內灣浪力較弱,如吐露港、鹽田梓、滘西洲、大潭港及欣澳長索。

Inner bays sheltered by headlands have weaker wave energy, such as Tolo Harbour, Yim Tin Tsai, Kau Sai Chau, Tai Tam Harbour and San Shek Wan at Yan O.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.280

沉積巖園區範圍涵蓋吐露港與大鵬灣地區。

The Sedimentary Rock Region covers the Tolo Harbour and Mirs Bay areas.

來源 《香港志·自然》自然環境(香港地方志中心) · p.239

此座地質公園由兩個主題園區組成,分別為火山岩園區及沉積巖園區;前者座落新界東部西貢一帶,後者則橫跨東北部吐露港兩岸與其周邊地帶。

This geopark consists of two themed areas, namely the volcanic rock area and the sedimentary rock area; the former is located around Sai Kung in eastern New Territories, while the latter spans both shores of Tolo Harbour in the northeast and its surrounding areas.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.117

大澳組的零星露頭亦可見於企嶺下海、深涌,以及中文大學附近一帶(位於新界吐露港)。

Sporadic outcrops of the Tai O Formation can also be seen at Kei Ling Ha Hoi, Sham Chung, and the area near the Chinese University (at Tolo Harbour in the New Territories).

來源 《香港志·自然》自然環境(香港地方志中心) · p.97

大鵬灣、牛尾海,連同吐露港及赤門水質管制區,均屬於東部水域的範圍。

Mirs Bay, Port Shelter, together with Tolo Harbour and Tolo Channel Water Control Zones, all fall within the eastern waters.

來源 《香港志·自然》環境保護與生態保育(香港地方志中心) · p.375

低浪沙灘沙粒較幼、沙面平坦,物種較多,如大嶼山水口和吐露港海星灣。

Low-wave beaches have finer sand and flatter surfaces with more species, such as Shui Hau on Lantau and Starfish Bay in Tolo Harbour.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.282

浪力較弱的沙灘包括吐露港海星灣及南大嶼山水口。

Beaches with weaker wave action include Hoi Sing Wan in Tolo Harbour and Shui Hau on South Lantau.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.282

林村河的下游河段,起自大埔頭抽水站東側,一路通往吐露港,目前該處已受人工整治,昔日天然地貌已消失。

The lower course of the Lam Tsuen River starts from the east side of the Tai Po Tau pumping station and runs to Tolo Harbour, where it has been artificially channelised and the former natural landform has disappeared.

來源 《香港志·自然》自然環境(香港地方志中心) · p.443

馬屎洲位於吐露港,屬大埔區,面積0.53平方公里。

Ma Shi Chau is located in Tolo Harbour, belongs to Tai Po District, and has an area of 0.53 square kilometres.

來源 《香港志·自然》自然環境(香港地方志中心) · p.646

吐露港、西貢海以及大鵬灣周邊水域,均屬於東部大洋型海區的範圍。

Tolo Harbour, Sai Kung Hoi, and the waters around Mirs Bay all fall within the eastern oceanic-type sea area.

來源 《香港志·自然》自然環境(香港地方志中心) · p.499

吐露港北面的赤門海峽,深度朝東北方向遞增。

The depth of Tolo Channel north of Tolo Harbour increases towards the northeast.

來源 《香港志·自然》自然環境(香港地方志中心) · p.54

吐露港地下水匯水盆地規模居香港之首,佔地約160平方公里。

The groundwater catchment basin of Tolo Harbour is the largest in Hong Kong, covering about 160 square kilometres.

來源 《香港志·自然》自然環境(香港地方志中心) · p.457

吐露港東岸深涌角和南岸泥涌均有赤門組出露,岩石含侏羅紀菊石化石。

The Chimeng Formation crops out at Deep Bay Point on the eastern shore of Tolo Harbour and at Nai Chung on the southern shore, and the rocks contain Jurassic ammonite fossils.

來源 《香港志·自然》自然環境(香港地方志中心) · p.97

吐露港附近的巖岸主要由砂岩構成,其岩石結構疏鬆,且具有較高的孔隙率。

The rocky coast near Tolo Harbour is mainly composed of sandstone, whose rock structure is loose and has a relatively high porosity.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.279

吐露港附近每年錄得約2400毫米平均降雨量,該匯水盆地年均可匯集約3.84億立方米雨水。

Average annual rainfall near Tolo Harbour is about 2,400 millimetres, and the catchment basin collects about 384 million cubic metres of rainwater annually.

來源 《香港志·自然》自然環境(香港地方志中心) · p.457

吐露港水深介於5米至15米,屬較淺海灣。

Tolo Harbour has a water depth of between 5 and 15 metres and is a relatively shallow bay.

來源 《香港志·自然》自然環境(香港地方志中心) · p.54

吐露港沿岸岩石以砂岩為主,質地較鬆散且孔隙度高。

The rocks along the coast of Tolo Harbour are mainly sandstone, which is relatively loose and highly porous.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.280

吐露港一帶每年平均雨量約2400毫米,其匯水盆地年均可收集約3.84億立方米雨水,約20%經下滲成為地下水,即約0.77億立方米。

The average annual rainfall around Tolo Harbour is about 2,400 mm; its catchment can collect about 384 million cubic metres of rainwater annually, of which about 20% becomes groundwater through infiltration, amounting to about 77 million cubic metres.

來源 《香港志·自然》自然環境(香港地方志中心) · p.457

吐露區巖岸風浪區長度介乎21.3至56.2公里。

The length of the rocky shore wave zone in the Tolo area ranges from 21.3 to 56.2 kilometres.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.280

吐露一帶的岩石組合包含粉砂岩、砂岩、黑雲母花崗巖及水晶凝灰岩。

The rock assemblage in the Tolo area includes siltstone, sandstone, biotite granite and crystal tuff.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.280

梧桐寨瀑布屬林村河上游,河水經林村谷最終注入吐露港。

Ng Tung Chai Waterfall belongs to the upper reaches of Lam Tsuen River, whose water flows through Lam Tsuen Valley and finally into Tolo Harbour.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.113

香港的紅樹林約有60個,合計面積約600公頃,分佈範圍涵蓋西貢、新界東北與吐露港,以及后海灣、大嶼山和香港島,共六個區域。

Hong Kong has about 60 mangrove sites with a total area of about 600 hectares, distributed across six regions covering Sai Kung, northeastern New Territories and Tolo Harbour, as well as Deep Bay, Lantau Island and Hong Kong Island.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.536

香港境內存在不少於五個具規模的地下水匯水盆地,吐露港與東涌的匯水盆地均屬其中。

There are no fewer than five sizable groundwater catchment basins in Hong Kong, including those of Tolo Harbour and Tung Chung.

來源 《香港志·自然》自然環境(香港地方志中心) · p.457

丫洲位於吐露港,屬大埔區,面積0.035平方公里。

A Chau is located in Tolo Harbour, belongs to Tai Po District, and has an area of 0.035 square kilometres.

來源 《香港志·自然》自然環境(香港地方志中心) · p.648

鹽田仔組岩石分佈範圍廣,吐露港一帶為主要出露地,另見於大嶼山、南丫島及港島南端。

Rocks of the Yim Tin Tsai Formation are widely distributed, with the Tolo Harbour area as the main outcrop, and are also found on Lantau Island, Lamma Island and the southern tip of Hong Kong Island.

來源 《香港志·自然》自然環境(香港地方志中心) · p.101

由吐露港北岸延伸至大鵬灣一帶,加上黃竹角咀半島與大埔八仙嶺,這些單斜山的地貌皆按照沉積巖的層理發育而成。

From the northern shore of Tolo Harbour to the Mirs Bay area, together with the Wong Chuk Kok Tsui peninsula and the Pat Sin Leng range in Tai Po, these cuesta landforms have developed in accordance with the bedding of sedimentary rocks.

來源 《香港志·自然》自然環境(香港地方志中心) · p.43

由五代南漢起,歷經清康熙時期,官方於大步海(即現今吐露港附近)進行珍珠採集,並設立相關部門負責監管。

From the Five Dynasties Southern Han through the Kangxi period of the Qing, the authorities collected pearls at Dabu Sea (near present-day Tolo Harbour) and set up a department to oversee it.

來源 《香港志·自然》建置與地區概況(人口)(香港地方志中心) · p.527

於五代十國階段,南漢政權在吐露港成立媚川都,專門負責珍珠採集事宜。

During the Five Dynasties and Ten Kingdoms period, the Southern Han regime established Meichuan Du at Tolo Harbour to take charge of pearl gathering.

來源 《香港志·自然》建置與地區概況(人口)(香港地方志中心) · p.23

在五代十國年間,南漢政權於屯門鎮設置軍隊戍守,同時把大步海(即現今吐露港)列作採集珍珠的關鍵區域。

During the Five Dynasties and Ten Kingdoms period, the Southern Han regime stationed troops at Tuen Mun Town and designated Tai Po Hoi (present-day Tolo Harbour) as a key area for pearl collection.

來源 《香港志·自然》建置與地區概況(人口)(香港地方志中心) · p.232

城門組及荔枝莊組的流紋巖,其石英晶體最大達7毫米,鉀長石與斜長石晶體則以3毫米為上限。

In the rhyolites of the Shing Mun Formation and the Lai Chi Chong Formation, quartz crystals reach up to 7 mm, while potassium feldspar and plagioclase crystals are limited to 3 mm.

來源 《香港志·自然》自然環境(香港地方志中心) · p.161

城門組岩石主要分佈於新界大帽山附近及吐露港以北。

The rocks of the Shing Mun Formation are mainly distributed near Tai Mo Shan in the New Territories and north of Tolo Harbour.

來源 《香港志·自然》自然環境(香港地方志中心) · p.102

城門組與荔枝莊組的流紋巖位於吐露港海峽南側,呈深灰色且厚度達35米。

The rhyolite of the Shing Mun Formation and Lai Chi Chong Formation is located on the southern side of the Tolo Harbour channel, is dark grey, and reaches a thickness of 35 metres.

來源 《香港志·自然》自然環境(香港地方志中心) · p.161

赤門海峽以北的泥盆紀岩石形成東北走向山脊,從吐露港伸展至黃竹角咀。

The Devonian rocks north of Tolo Channel form a northeast-trending ridge extending from Tolo Harbour to Wong Chuk Kok Tsui.

來源 《香港志·自然》自然環境(香港地方志中心) · p.92

二疊紀大埔海組的主要露頭,分佈於吐露港內的馬屎洲及丫洲一帶。

The main outcrops of the Permian Tai Po Hoi Formation are distributed around Ma Shi Chau and Yau Chau in Tolo Harbour.

來源 《香港志·自然》自然環境(香港地方志中心) · p.96

飛白楓海星常見於吐露港一帶,部分個體只有四隻腕。

Protoreaster nodosus is commonly found around Tolo Harbour, and some individuals have only four arms.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.429

根據估算,吐露港一帶的鹽田仔組地層約有200米厚,並以覆蓋方式位於侏羅紀赤門組的沉積巖層之上。

It is estimated that the Yim Tin Tsai Formation around Tolo Harbour is about 200 metres thick and lies conformably over the sedimentary rocks of the Jurassic Tolo Channel Formation.

來源 《香港志·自然》自然環境(香港地方志中心) · p.102

海草牀可見於大嶼山䃟頭、流浮山白泥,以及荔枝窩與吐露港等區域。

Seagrass beds can be found at San Tau on Lantau Island, Pak Nai at Lau Fau Shan, and areas such as Lai Chi Wo and Tolo Harbour.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.277

紅石門、往灣洲一帶、東平洲及吐露港內海可找到珊瑚群落。

Coral communities can be found at Red石門, the area around Wong Wan Chau, Tung Ping Chau and the inner sea of Tolo Harbour.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.293

磯沙蠶科一種物種於吐露港附近水域錄得,其名稱源自香港。

A species of the family Eunicidae was recorded in waters near Tolo Harbour, and its name derives from Hong Kong.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.445

引用名稱學名 Marphysa hongkongensa

龍鼓灘與吐露港等昔日馬蹄蟹分佈地,現已不見馬蹄蟹,后海灣數量亦大幅下降。

Horseshoe crabs are no longer found at former distribution sites such as Lung Kwu Tan and Tolo Harbour, and their numbers in Deep Bay have also dropped sharply.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.401

全港泥灘數量不少於四十九個,主要分佈於吐露港與西面沿岸一帶。

There are no fewer than 49 mudflats in Hong Kong, mainly distributed around Tolo Harbour and along the western coast.

來源 《香港志·自然》自然環境(香港地方志中心) · p.501

湯森針對海膽以及吐露港珊瑚礁範圍內的棘皮動物進行探究,其研究成果在莫雅頓所舉辦的海洋生物研討會上對外發表。

Townsend studied sea urchins and echinoderms within the coral reef areas of Tolo Harbour, and the findings were presented at a marine biology symposium held in Mordialloc.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.428

吐露港、西貢內海鹽田梓、滘西洲及大潭港等地有浪力弱小的巖岸。

Rocky shores with weak wave action are found at Tolo Harbour, the inner sea of Sai Kung at Yim Tin Tsai, Kau Sai Chau and Tai Tam Harbour.

來源 《香港志·自然》自然環境(香港地方志中心) · p.500

吐露港海星灣及南大嶼水口等內灣沙灘浪力較弱,沙粒較幼。

Sheltered bay beaches such as Starfish Bay in Tolo Harbour and Shui Hau on south Lantau have weaker wave action and finer sand.

來源 《香港志·自然》自然環境(香港地方志中心) · p.501

吐露港海星灣偶爾可見細小且間歇出現的海草群落。

Small and intermittent seagrass communities are occasionally seen at Starfish Bay in Tolo Harbour.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.291

吐露港及香港東北沿岸因地形相對封閉,其波浪作用較東部與東南部海岸為弱。

Because of the relatively enclosed topography of Tolo Harbour and the northeastern coast of Hong Kong, wave action there is weaker than on the eastern and southeastern coasts.

來源 《香港志·自然》自然環境(香港地方志中心) · p.499

吐露港馬屎洲西北岸與鹽田仔洲東南岸,可見鹽田仔組底部30多米厚角礫巖層。

On the northwestern shore of Ma Shi Chau and the southeastern shore of Yim Tin Tsai in Tolo Harbour, a basal breccia layer more than 30 m thick of the Yim Tin Tsai Formation can be seen.

來源 《香港志·自然》自然環境(香港地方志中心) · p.102

吐露港內老圍、榕樹澳、西徑及瓦窰頭等地有多處泥灘。

There are several mudflats at Lo Wai, Yung Shue O, Sai Keng and Nga Yiu Tau in Tolo Harbour.

來源 《香港志·自然》自然環境(香港地方志中心) · p.501

吐露港毗鄰白沙頭洲,而該洲處於黃竹角咀半島西南方向的最末端位置。

Tolo Harbour is adjacent to Pak Sha Tau Chau, which is at the southwesternmost end of the Wong Chuk Kok Tsui Peninsula.

來源 《香港志·自然》自然環境(香港地方志中心) · p.92

吐露港一帶海草分佈於海星灣和汀角。

Seagrasses in Tolo Harbour are distributed at Starfish Bay and Ting Kok.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.292

吐露港一帶沙泥灘和紅樹林可觀察到擬蟹守螺爬樹現象。

Tree-climbing behaviour of Cerithidea species can be observed on the sandy mudflats and mangroves around Tolo Harbour.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.420

吐露港至西貢北一帶昔日盛產企鵝鶯蛤與凹珠母蛤。

The area from Tolo Harbour to North Sai Kung was formerly rich in penguin wing oysters and concave pearl oysters.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.425

一戰後,韓雷在吐露港北岸赤門海峽一帶鳳凰笏沉積巖地層發現菊石化石與雙殼類化石。

After World War I, Han Lei discovered ammonite and bivalve fossils in the sedimentary strata at Fung Wong Wat along the Tolo Channel on the northern shore of Tolo Harbour.

來源 《香港志·自然》自然環境(香港地方志中心) · p.226

玉足海參與棕環參被騷擾時會噴出居維氏管纏繞捕獵者。

Holothuria leucospilota and Stichopus chloronotus eject Cuvierian tubules to entangle predators when disturbed.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.429

雜色角孔海膽常見於吐露港下潮帶的沙泥基質。

Echinometra mathaei is commonly found on sandy-mud substrates in the lower intertidal zone of Tolo Harbour.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.429

在吐露港馬屎洲、荔枝莊及港島大潭港等浪力較低的巖岸,可見體型較長的螺類。

On lower-energy rocky shores such as Ma Shi Chau and Lai Chi Chong in Tolo Harbour and Tai Tam Harbour on Hong Kong Island, longer-bodied snail species can be seen.

來源 《香港志·自然》自然資源與生態(香港地方志中心) · p.419

在吐露港馬屎洲可看到大埔海組巖層兩種明顯不同的巖相。

Two distinctly different rock facies of the Tai Po Sea Formation can be seen at Ma Shi Chau in Tolo Harbour.

來源 《香港志·自然》自然環境(香港地方志中心) · p.96

鶴佬人聚居於新界東部沿海及離島,如吐露港、長洲、坪洲。

Hoklo people settled along the eastern coast of the New Territories and on outlying islands such as Tolo Harbour, Cheung Chau and Peng Chau.

來源 《香港志·自然》建置與地區概況(人口)(香港地方志中心) · p.295

來源 Sources

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