Hong Kong's main stock market index, the HK50, fell to 23961 points on July 3, 2025, losing 1.08% from the previous session. Over the past month, the index has climbed 1.30% and is up 32.91% compared to the same time last year, according to trading on a contract for difference (CFD) that tracks this benchmark index from Hong Kong. Hong Kong Stock Market Index (HK50) - values, historical data, forecasts and news - updated on July of 2025.

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The interferences from GeoLa- GK50 are shown.

The distribution of the hydrogeological top layers is shown. A top layer is a near-surface hydrogeological unit above the first contiguous groundwater body, which does not contain any significant groundwater in its entirety, with the exception of floating groundwater. It is completely in the area of the unsaturated zone. In the foothills of the Alps, the glacial sediments were not classified as top layers. The classification of the top layers is based on their permeability.

Dargestellt ist der hydrogeochemische Gesteinstyp der an der Erdoberfläche verbreiteten hydrogeologischen Einheiten, der für die Wirkung auf den Chemismus des darin auftretenden Grundwassers maßgeblich sind.

The pages of the hydrogeological map [HK 50] of North Rhine-Westphalia on a scale of 1 : 50,000 show the distribution, location and rock composition of the aquifers and aquifers occurring in the map area. In the main maps, loose and solid rock are assigned to different permeability classes according to their hydraulic properties. In the loose rock, the thickness of the usable groundwater space is also shown. The maps also contain information on the location of springs, wells, groundwater measuring points and potential groundwater hazards (excavations, embankments). Hydrogeological series of sections give an impression of the position, the thickness and the hydraulic connections of the hydrogeological units. In newer sheets, another map shows the distribution and composition of overlying layers and their protective function for the groundwater, the risk of substances entering the groundwater is classified. Information on geogenic groundwater quality is also given here. Additional maps (e.g. geological overview, quaternary basis and permeability of the surface layers, groundwater analyzes or basic processing) are partially included. The construction of the groundwater surface - also shown on an inset map - is based on digital data from the State Environment Agency of North Rhine-Westphalia (LUA), Essen. Additional information about groundwater levels and water protection areas can be obtained there. Some of the map sheets are accompanied by short explanations with a list of publications, in which the focus is on the content and presentation of the maps as well as on groundwater management and the prospects of the strata occurring in the map area. Publications: Hydrogeological map 1: 50,000 sheets, year of publication L 4318 Paderborn, 1970 as a print [with abbreviation] L 3510 Freren/Bramsche, 2001 as a print L 3708 Gronau (Westphalia), 1993 as a print [with abbreviation] L 3710 Rheine , 1983 as a print [with abbreviation] L 3712 Ibbenbüren, 2001 as a print, as a plot (also digital) L 3906 Vreden, 1982 as a print L 3908 Ahaus, 1981 as a print L 3910 Steinfurt, 1997 as a print (also digital) L 3912 Lengerich, 1996 as a print (also digital) L 3914 Bad Iburg 2006 as a print, as a plot (also digital) L 3918 Herford, 1984 as a print [with abbreviation] L 4116 Gütersloh, 2000 as a print, as a plot (also digital) L 4118 Detmold, 1987 as a print [with abbreviation] L 4314 Beckum, 1999 as a print (also digital) L 4316 Lippstadt 2006 as a print, as a plot (also digital) L 4318 Paderborn, 1984 as a print [with abbreviation] L 4514 Soest , 2003 as a print, as a plot (also digital) L 5110 Waldbröl, 1985 as a print

Shown are the classes of the mean horizontal mountain permeability of the hydrogeological units spread on the earth’s surface without cover layers (classification scheme according to the Hydrogeological mapping guide, Ad-Hoc-AG Hydrogeology 1997) In sufficient data, the classification is based on the determination of the permeability from pumping tests, in the remaining cases on experience. The qualitative data on the permeability of the cohesive top layers were estimated on the basis of their lithological training. If the mountain permeability of a hydrogeological unit comprises two classes, it receives the colouring of the class with the lower permeability, it comprises three classes it receives the colouring of the middle class. Further information can be found at https://services.lgrb-bw.de/resources/link/hyd/geola_hyd_durch.pdf

The hydrogeological map of North Rhine-Westphalia on a scale of 1:50.000 [HK 50] shows the distribution, location and rock characteristics of the aquifers and low-level aquifers found in the leaf area. In the cards, looser and solid rocks are assigned different permeability classes according to their hydraulic properties; the width of the usable groundwater space is also shown in the loose rock. The maps also contain information on the location of springs, wells, groundwater monitoring stations and potential groundwater hazards (excavations, deposits). Cutting series give an impression of the storage, width and hydraulic connections of the hydrogeological units.

The distribution of hydrogeological units (including cohesive top layers) on the Earth’s surface is shown. A hydrogeological unit is a rock body that, due to its petrography, texture or structure, has uniform hydrogeological properties within a defined range. A top layer is a near-surface hydrogeological unit above the first contiguous groundwater body, which does not contain any significant groundwater in its entirety, with the exception of floating groundwater. It is completely in the area of the unsaturated zone. The bandwidth within which a rock body is considered homogeneous is strongly dependent on the processing and representation scale (Ad-Hoc-AG Hydrogeology). The basic hydrogeological map is derived from the basic digital geological data set. For the determination of the hydrogeological units, the geological mapping units are divided according to hydrogeological aspects (lithofazies, hydrogeological and geochemical properties).

Key information about Hong Kong SAR (China) P/E ratio

• Hong Kong SAR (China) Hang Seng recorded a daily P/E ratio of 11.950 on 26 Mar 2025, compared with 12.200 from the previous day.
• Hong Kong SAR (China) Hang Seng P/E ratio is updated daily, with historical data available from Apr 2000 to Mar 2025.
• The P/E ratio reached an all-time high of 18.400 in Nov 2010 and a record low of 7.450 in Feb 2016.
• Hang Seng Indexes Company Limited provides daily P/E Ratio.

Interactive daily chart of the Hong Kong Hang Seng Composite stock market index back to 1986. Each data point represents the closing value for that trading day and is denominated in hong kong dollars (HKD). The current price is updated on an hourly basis with today's latest value.

Prices for HK50 - Prix De L'Action including live quotes, historical charts and news. HK50 - Prix De L'Action was last updated by Trading Economics this July 4 of 2025.

Dargestellt ist die flächenhafte Verbreitung mächtigerer, überwiegend sandig kiesiger quartärer Lockergesteine (Porengrundwasserleiter, PGWL) . In diesen Ablagerungen ist grundsätzlich mit Grundwasservorkommen zu rechnen. Die ausgewiesenen Porengrundwasserleiter lassen in Verbindung mit der hydrogeologischen Karte ohne Deckschichten einen Kontakt eines Festgesteinsgrundwasserleiters mit einem Porengrundwasserleiter erkennen und können damit Hinweise auf eine mögliche Wechselbeziehung zwischen den Grundwasserkörpern in diesen Einheiten geben (außer im Oberrheingraben und im Alpenvorkand).

Prices for HK50 - Prezzo Delle Azioni including live quotes, historical charts and news. HK50 - Prezzo Delle Azioni was last updated by Trading Economics this June 20 of 2025.

Dargestellt sind die Klassen der mittleren horizontalen Gebirgsdurchlässigkeit der an der Erdoberfläche verbreiteten hydrogeologischen Einheiten ohne Deckschichten (Klassifikationsschema nach der Hydrogeologischen Kartieranleitung, Ad-Hoc-AG Hydrogeologie 1997) Bei ausreichender Datengrundlage basiert die Klassifizierung auf der Bestimmung der Durchlässigkeiten aus Pumpversuchen, in den übrigen Fällen auf Erfahrungswerten. Die qualitativen Angaben zur Durchlässigkeit der bindigen Deckschichten wurden anhand ihrer lithologischen Ausbildung abgeschätzt. Umfasst die Gebirgsdurchlässigkeit einer hydrogeologischen Einheit zwei Klassen, erhält sie die Farbgebung der Klasse mit der niedrigeren Durchlässigkeit, umfasst sie drei Klassen erhält sie die Farbgebung der mittleren Klasse. Weitere Angaben unter https://services.lgrb-bw.de/resources/link/hyd/geola_hyd_durch.pdf

Dargestellt ist der Grundwasserleitertyp der an der Erdoberfläche verbreiteten hydrogeologischen Einheiten. Grundwasserleiter (GWL) sind hydrogeologische Einheiten, die aufgrund ihres Gehalts an Hohlräumen in der Lage sind, Grundwasser weiter zu leiten (Durchlässigkeit kf >= 1 * 10-5 m/s). Grundwassergeringleiter sind hydrogeologische Einheiten, die Grundwasser nur in sehr geringem Umfang weiter leiten können (Durchlässigkeit kf < 1 * 10-5 m/s).

Az NDK hidrogeológiai térképe: 50 000 (HK50), csarnok 1987

Kvaterner víztartó rétegek: Hidrogeológiai térképek, hidrogeológiai jellemzők térképek, hidroizohyps térképek, felszín alatti vizek veszélytérképei

Harmadlagos víztartó rétegek: Hidrogeológiai térképek

Die Hydrogeologische Karte von Nordrhein-Westfalen im Maßstab 1:50.000 [HK 50] zeigt Verbreitung, Lage und Gesteinsbeschaffenheit der im Blattgebiet vorkommenden Grundwasserleiter und -geringleiter. In den Karten sind Locker- und Festgesteine entsprechend ihrer hydraulischen Eigenschaften verschiedenen Durchlässigkeitsklassen zugeordnet; im Lockergestein ist zusätzlich die Mächtigkeit des nutzbaren Grundwasserraumes wiedergegeben. Ferner enthalten die Karten Angaben zur Lage von Quellen, Brunnen, Grundwassermessstellen und potenziellen Grundwassergefährdungen (Abgrabungen, Aufschüttungen). Schnittserien vermitteln einen Eindruck über die Lagerung, die Mächtigkeit und die hydraulischen Verbindungen der hydrogeologischen Einheiten.