Untitled-1-Recovered

Belitung

Indonesia

Southern Tin Granite Beaches

Untitled-1-Recovered

Toba Caldera National Geopark

Sumatra Utara Indonesia

Super Volcano eruption, Caldera Landscape development

Lake Toba is situated in Sumatera Island, formed by a mega-volcanic eruptions 74,000 years ago, is the largest with-in the Quaternary. It is the ‘super volcano’ eruption (VEI> 8) which produced 2,800 km³ pyroclastics materials, where 2,000 km³ of volcanic-ash dispersed to W-NW directions, and also distributes of sulfuric-acid aerosol to the atmosphere which is deposited in the Antartic areas. The environment of Lake Toba region with a particular micro-climate environment, have ‘endemic’ flora and fauna ecosystem, and also the various Batak Cultures which reflects the local-wisdom.

Untitled-1-Recovered

Merangin Geopark

Jambi Indonesia

Ancient Permian Jambi flora capped by Volcanic processes and fluvial processes.

Merangin Geopark, located in Merangin Regency, Jambi Province, has an area of 1,699 km2, with wide distribution of Jambi flora fossils of 290 million years old. The fossil is a proof that the old land Merangin be evidence of the spread of Cathaysian flora, and became a reference in every reconstruction of plate movement.

Untitled-1-Recovered

Ciletuh-Palabuharatu Geopark

Jawa Barat Indonesia

Subduction zone uplifted rocks, Jampang Plateau landscape, Ancient magmatic zone shifting, Fore arc evolution.

Ciletuh-Palabuhanratu Geopark is located in Sukabumi Regency, West Jawa Province, Indonesia. This Geopark has an outstanding geological features of oldest rock formation, horseshoe-shaped landscape and geyser; biodiversity of rafflesia padma; and culture diversity such as the traditional agriculture and rice harvest thanksgiving ceremony known as Seren Taun and heritage site of Megalithic era.

Untitled-1-Recovered

Rinjani Geopark

Nusa Tenggara Barat Indonesia

Recent Caldera Landscape & its active volcano formation

Rinjani Geopark is part of the province of West Nusa Tenggara . It has extensive delineation ± 2,800 km2 , covering 5 districts / cities : distric of North Lombok, district of East Lombok , district of Central Lombok, district of West Lombok and Mataram City. It has a potential 22 geo diversities, 8 bio diversities, and 17 culture diversities that make Lombok Geopark Rinjani becomes leading tourism destination In Lombok Island. Collaboration between government as steering function and society as executive function is a key in the development of Lombok Geopark Rinjani. Community empowerment as actor in the management gives the effect of increasing prosperity that is continuously improved in terms of knowledge, skills, and mentoring.

Untitled-1-Recovered

Gunung Sewu Geopark

Yogyakarta – Jawa Tengah Indonesia

Conical Karst landscape with extensive caves, Uplifted beaches

Became a UNESCO Global Geopark on September 19, 2015, Gunung Sewu is a showcase of high aesthetic value of tropic conical karst landscapes in southern part of Java. The closely related between geodiversity and endemic flora-fauna, ecosystems, as well as intangible cultures diversities is an Earth’s heritage that formed a complete history of area of 40 million years ago until now. Prehistoric man who ever lived together with rhinos and hippos that now extinct is a portrait of the circumstances of about 10,000-4,000 years ago. The locals experience benefits of Geopark from geotourism, education, and education aspects.

Untitled-1-Recovered

Batur Geopark

Bali Indonesia

Caldera landscape evolution, with pyroclastic surge and strombolian type eruption and high temperature lava flows

Located in northern part of Bali, Indonesia, Batur active volcano with its double-calderas has a very beuatiful lanscape phenomenon. Landscape of double-calderas, active volcanic cones, lake, lava flows, cinder cones and maar is a unified volcanic morphology that became a history of the dynamics of volcanism phenomenon over tens of thousands years ago to present time. “Caldera in caldera” that is rarely found elsewhere.

Untitled-1-Recovered

Lembah Harau

Sumatra Barat, Indonesia

Landscape of Great Sumatra fault and its extensional tectonic activities

Untitled-1-Recovered

Pongkor

Indonesia

Untitled-1-Recovered

Pangandaran

Indonesia

Pangandaran is a town and district of Pangandaran Regency within the province of West Java, Indonesia. It is located on the southern coast of the island of Java. Awell-known surfing beach has made Pangandaran a popular tourist destination.

Untitled-1-Recovered

Karang Sambung

Karst Gombong Selatan – Kebumen, Indonesia

Subduction zone uplifted rocks combined with conical hills landscape formation in fore arc region

Untitled-1-Recovered

Dieng

Indonesia

Highland Mountainous Landscape formed by Recent volcanic activities

Dieng Plateau is a marshy plateau that forms the floor of a caldera complex on the Dieng Volcanic Complex near Wonosobo, Central Java, Indonesia.[1] Referred to as “Dieng” by Indonesians, it sits at 2,000 metres (6,600 ft) above sea level, far from major population centres. The name “Dieng” comes from Di Hyang which means “Abode of the Gods”.

Untitled-1-Recovered

Bromo

Indonesia

Widespread dry land sandy caldera formed by Recent volcanic

Mount Bromo (Indonesian: Gunung Bromo), is an active volcano and part of the Tengger massif, in East Java, Indonesia. At 2,329 metres (7,641 ft) it is not the highest peak of the massif, but is the most well known. The massif area is one of the most visited tourist attractions in East Java, Indonesia. The volcano belongs to the Bromo Tengger Semeru National Park. The name of Bromo derived from Javanese pronunciation of Brahma, the Hindu creator god.

Untitled-1-Recovered

Ijen

Indonesia

The Ijen volcano complex is a group of stratovolcanoes in the Banyuwangi Regency of East Java, Indonesia. It is inside a larger caldera Ijen, which is about 20 kilometers wide. The Gunung Merapi stratovolcano is the highest point of that complex. The name “Gunung Merapi” means “mountain of fire” in the Indonesian language (api being “fire”); Mount Merapi in central Java and Marapi in Sumatra have the same etymology.

Untitled-1-Recovered

Tambora

Indonesia

Recent catasthropic Plinian eruption with gigantic pyroclastic flows

Untitled-1-Recovered

Kelimutu

Indonesia

Untitled-1-Recovered

Maros Pangkep

Sulawesi Selatan, Indonesia

The development Miocene Tower and table karst landscape

Maros is a town in the South Sulawesi province of Indonesia close to the provincial capital of Makassar. It is the capital of the Maros Regency. Maros is the location of the Indonesian Cereals Research Institute, a branch of the Indonesian Agency for Agricultural Research and Development.

Untitled-1-Recovered

Toraja

Indonesia

Untitled-1-Recovered

Sangkuriang

Indonesia

Untitled-1-Recovered

Tondano

Indonesia

Mount Tondano in the province of North Sulawesi, Sulawesi, Indonesia, has a 20 × 30 km wide caldera which was formed in the Late Miocene or Early Pliocene[2] formed by a massive eruption. Post caldera activity includes Pyroclastic cones, obsidian flows and geothermal areas in the caldera area. The Lake Tondano lies in the east side of the caldera.

Untitled-1-Recovered

Raja Ampat

Papua Barat Indonesia

Island karst landscape, Recent Active uplifted widespread platform

Located off the northwest tip of Bird’s Head Peninsula on the island of New Guinea, in Indonesia’s West Papua province, Raja Ampat, or the Four Kings, is an archipelago comprising over 1,500 small islands, cays, and shoals surrounding the four main islands of Misool, Salawati, Batanta, and Waigeo, and the smaller island of Kofiau. The Raja Ampat archipelago is the part of Coral Triangle which contains the richest marine biodiversity on earth.

error: Content is protected !!