Todd Carmichael travels the globe, hunting for the highest-grade coffee in the world. Why? Because nearly a billion people drink coffee each morning, making it the number 2 commodity in the world, second only to oil.
Todd focuses on the very best coffee out there. Beans so rare, they are sought after by the world's top chefs and restaurants. Todd has to go to some of the most exotic, fascinating and dangerous places on earth to find it: from the cities, villages and mountains of Haiti, Bolivia, Madagascar, Borneo, Cuba and Vietnam. Buying the coffee beans direct from the farmers means Todd must encounter treacherous terrain, danger and sometimes, even opposition from entrenched middlemen. There's an amazing story behind every cup.
Runtime: 60 minutes
Dangerous Grounds - Spratly Islands - Netflix
The Spratly Islands (Chinese: 南沙群岛 (Nánshā Qúndǎo), Malay: Kepulauan Spratly, Tagalog: Kapuluan ng Kalayaan, Vietnamese: Quần đảo Trường Sa) are a disputed group of islands, islets and cays and more than 100 reefs, sometimes grouped in submerged old atolls, in the South China Sea. The archipelago lies off the coasts of the Philippines, Malaysia, and southern Vietnam. Named after the 19th-century British whaling captain Richard Spratly who sighted Spratly Island in 1843, the islands contain less than 2 km2 (490 acres) of naturally occurring land area spread over an area of more than 425,000 km2 (164,000 sq mi). The Spratlys are one of the major archipelagos in the South China Sea which complicate governance and economics in this part of Southeast Asia due to their location in strategic shipping lanes. The islands have no indigenous inhabitants, but offer rich fishing grounds and may contain significant oil and natural gas reserves, and as such are important to the claimants in their attempts to establish international boundaries. Some of the islands have civilian settlements, but of the approximately 45 islands, cays, reefs and shoals that are occupied, all contain structures that are occupied by military forces from Malaysia, Taiwan (ROC), China (PRC), the Philippines and Vietnam. Additionally, Brunei has claimed an exclusive economic zone in the southeastern part of the Spratlys, which includes the uninhabited Louisa Reef.
Dangerous Grounds - Geology - Netflix
The Spratly Islands consist of islands, reefs, banks and shoals that consist of biogenic carbonate. These accumulations of biogenic carbonate lie upon the higher crests of major submarine ridges that are uplifted fault blocks known by geologists as horsts. These horsts are part of a series of parallel and en echelon, half-grabens and rotated fault-blocks. The long axes of the horsts, rotated fault blocks and half-grabens form well-defined linear trends that lie parallel to magnetic anomalies exhibited by the oceanic crust of the adjacent South China Sea. The horsts, rotated fault blocks, and the rock forming the bottoms of associated grabens consist of stretched and subsided continental crust that is composed of Triassic, Jurassic, and Cretaceous strata that include calc-alkalic extrusive igneous rocks, intermediate to acid intrusive igneous rocks, sandstones, siltstones, dark-green claystones, and metamorphic rocks that include biotite–muscovite–feldspar–quartz migmatites and garnet–mica schists. The dismemberment and subsidence of continental crust into horsts, rotated fault blocks and half-grabens that underlie the Spratly Islands and surrounding sea bottom occurred in two distinct periods. They occurred as the result of the tectonic stretching of continental crust along underlying deeply rooted detachment faults. During the Late Cretaceous and Early Oligocene, the earliest period of tectonic stretching of continental crust and formation of horsts, half-grabens, and rotated fault-blocks occurred in association the rifting and later sea-floor spreading that created the South China Sea. During the Late Oligocene-Early Miocene additional stretching and block faulting of continental crust occurred within the Spratly Islands and adjacent Dangerous Ground. During and after this period of tectonic activity, corals and other marine life colonised the crests of the horsts and other ridges that lay in shallow water. The remains of these organisms accumulated over time as biogenic carbonates that comprise the current day reefs, shoals and cays of the Spratly Islands. Starting with their formation in Late Cretaceous, fine-grained organic-rich marine sediments accumulated within the numerous submarine half-grabens that underlie sea bottom within the Dangerous Ground region. The geological surveys show localised areas within the Spratly Islands region are favourable for the accumulation of economic oil and gas reserves. They include thick sequences of Cenozoic sediments east of the Spratly Islands. Southeast and west of them, there also exist thick accumulations of sediments that possibly might contain economic oil and gas reserves lie closer to the Spratly Islands.
Dangerous Grounds - References - Netflix