Mountains the status of a separate mountain chain, in most other ways this chain is still considered the highest of all Dinaric areas, connected with the Dinaric mountain chain in terms of geology, morphology, and ethnography. Massifs The Accursed Mountains are made up of many large sections or mountain massifs/groups, all of which are connected to one another. These massifs include the Popluks group with a height of , the Shkurt group at , the Radohimës group at , the Zaborës e Krasniçës at , the Bjelic group at , the Karanfili-Brada group at , the Rabës group at , the Ershellit group at , the Kakinjes group at , the Shkëlzen group at , the Bogićevica group at , the Horolac group at , the Kershi Kocaj group at , the Maja e Zezë group at , the Lumbardhit group at , the Kopranik group at , the Strellc group at , the Gjeravica group at , the Junik group at , the Starac-Qokorr group , the Hajla group at , the Stedim-Ahmica group at , the Zleb-Rusulija group at , the Mokna group at and the Suva Planina group at . Canyons and valleys Erosion during glaciation left many telltale features behind. Deep river canyons and flat valleys wind around the ridges of the mountains. The largest canyon is Rugova Canyon. It is situated in Kosovo and is long from the border with Montenegro to Peja and is deep. It has very steep vertical mountain slopes on both sides. Valleys common at lower altitudes are found at the alpine level, creating mountain passes and valley troughs, such as Buni Jezerce in Albania. Buni Jezerce means "Valley of the Lakes" and it contains six small glacial lakes, the biggest being called the Big lake of Buni Jezerce. Canyons in the Accursed Mountains Rugova Canyon Deçani Canyon Gashi Canyon Cemi Canyon Valleys in the Accursed Mountains Vermosh Valley Valbona Valley Thethi Valley Ropojona Valley Gerbja Valley Buni Jezerce Cemi i Nikçit Valley Rivers and lakes The Accursed Mountains include many of the important rivers of the southeastern part of the Western Balkans. Rivers in this range fall roughly into two main categories, those that flow into the Lim and those that enter the White Drin and meet the Black Drin downstream at the Drin confluence. The southern and eastern slopes of the Accursed Mountains fall into the latter category. The